& Planetary Science 40, Nr 9, Supplement, A201–A263 (2005) http://meteoritics.org

The Meteoritical Bulletin, No. 89, 2005 September

Sara S. RUSSELL1*, Michael ZOLENSKY2, Kevin RIGHTER2, Luigi FOLCO,3 Rhian JONES,4 Harold C. CONNOLLY, JR.5, Monica M. GRADY1, 6, and Jeffrey N. GROSSMAN7

1Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK 2Code ST, NASA Johnson Space Center, Houston, Texas 77058, USA 3Museo Nazionale dell’Antartide, Via Laterina 8, I-53100 Siena, Italy 4Institute of Meteoritics, Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA 5Department of Physical Sciences, Kingsborough College and the Graduate School of CUNY, Brooklyn NY 11235, USA and Department of Earth & Planetary Science, American Museum of Natural History, Central Park West, New York 11024, USA 6Planetary and Space Sciences Research Institute, The Open University, Walton Hall, Milton Keynes, MK7 6AA, UK 7United States Geological Survey, MS 954, Reston, Virginia 20192, USA *Corresponding author. E-mail: [email protected] (Received 17 June 2005)

Abstract–This Bulletin lists 1768 , bringing the total known meteorites to over 30,000 at 30,907. Of these, 1010 are from Antarctica, 569 from Africa, 92 from Asia (83 of which are from Oman), 85 from North America, one from South America and 11 from Europe. The Bulletin reports seven falls (Benguerir, Bukhara, Kasauli, Maigatari-Danduma, Oum Dreyga, Rahimyar Khan, and San Michele). Noteworthy specimens include 20 lunar meteorites, four Martian meteorites, two , three , and two Bencubbin-like meteorites. Additional information can be found at http://meteoriticalsociety.org/bulletin/database.html.

INTRODUCTION NEWLY DESCRIBED METEORITES

The Meteoritical Bulletin publishes announcements by Acfer 360 27°29′N, 3°46′E the ’s Nomenclature Algeria Committee of newly described and classified meteorites. Found 2002, November 17 Several conventions are followed in this document. Shock () classifications conform to the scheme of Stöffler et al. A 68 g stone was found in the Acfer region of the Algerian (1991). The scale of Wlotzka (1993) is used to describe Sahara. Mineralogy and classification (E.-M. Chamorro, K. weathering grades, except as noted. For groups, Pistre, P. Beck, ENSL, P. Grandjean, UCB): the meteorite has petrologic types, shock stages, and weathering grades, a typical ureilite texture, mm-sized crystals, triple junctions, slashes (e.g., H5/6) indicate transitional assignments. and curved intergranular boundaries are observed. The Hyphens in petrologic type assignments for (e.g., mineral composition is olivine (Fo83) 90 vol%, pigeonite H5–6) indicate the range of types observed in . (En75Wo8) 8 vol% and interstitial carbonaceous material Group names such as “L(LL)” indicate uncertain 2 vol%. Olivine often contains metal inclusions, and assignments, with the less probable group in parentheses. pigeonite sometimes includes rounded olivine grains. Metal- The word “ungrouped” indicates that a meteorite can not be rich rims surround silicate grain boundaries. Flakes of dark, fit into existing classification schemes. The word carbonaceous material consist of diamonds in the form of “anomalous” is used if a meteorite can be assigned to an small grains within graphite, as revealed by Raman established class, but differs from other members of that spectroscopy. Weathering grade appears to be minor. class in a significant way. All italicized abbreviations refer to Specimens: main mass, F. Beroud and C. Boucher; type addresses tabulated at the end of this document. specimen 14 g, ENSL.

A201 © The Meteoritical Society, 2005. Printed in USA. A202 S. S. Russell et al.

African Meteorites Chen, NU. All type specimens and the remainder of the Table 1 lists 78 meteorites found at known locations in Africa. masses are at the Polar Research Institute of China, Shanghai.

American Meteorites Antarctic PSF Meteorites Table 2 lists 76 meteorites found in North and South America. (11 meteorites) Antarctica Antarctic ANSMET Meteorites Found 2002 (850 meteorites) Table 5 reports classification of 11 meteorites collected on the Antarctica blue ice at Pecora Escarpment by members of the Planetary Found 2002–2003 Studies Foundation’s Antarctica 2002 Expedition. Appendix 1 brings up to date the list of officially announced Classification: P. Sipiera, PSF. Specimens: Main mass and meteorites from the U.S. Antarctic Meteorite Program. Some type specimens, DuPont. 11,636 ANSMET meteorites have been listed in previous editions of The Meteoritical Bulletin; these meteorites bring Benguerir ~32°15′N, 08°09′W the total to 12,486. Listed are the classifications, masses, Morocco degrees of weathering, olivine and pyroxene compositions, Fell 2004 November 22, ~11:45 GMT pairing information, ice fields upon which the meteorites (LL6) were found, and bibliographic information—all sorted by A meteorite shower was witnessed to fall near Benguerir sample name. Meteorites were recovered from Dominion (~50 km due north of Marrakesh, Morocco) by local people on Range (DOM), MacAlpine Hills (MAC), Meteorite Hills 2004 November 22, at ~11:45 GMT. The fall had an east-to- (MET), Miller Range (MIL), Queen Alexandra Range west trajectory. The estimated total recovered mass is ~25– (QUE), La Paz Ice Field (LAP), Pecora Escarpment (PCA), 30 kg. Three stones fell at the following localities: Douar Roberts Massif (RBT), and Sandford Hills (SAN). The Lfokra (32°13′52.9′′N, 08°08′56.7′′W), Ahl Fouim Sakhra meteorites in Appendix 1 were published in The Antarctic Lourania (32°15′31.2′′N, 08°10′51.9′′W) and Douar Tnaja Meteorite Newsletter (AMN) issues 27(2) (2004) and 28(1) (32°15′43.1′′N, 08°09′01.3′′W). Two additional stones were (2005). Brief descriptions of meteorites other than also found further west, near Si Abdellah and Tnine equilibrated ordinary chondrites are published in AMN. Note Bouchane. A stone weighing ~4 kg, possibly recovered at meteorite pairings may be tentative. Douar Tnaja, shows dull, black fusion crust and regmaglypts on one side, and it is presently held at the office of the Antarctic PNRA Meteorites Governor of the Kelaa Sraghna Province. Another stone (98 meteorites) weighing ~1.2 kg, possibly from Douar Lfokra, is kept in the Antarctica laboratory of the Gendarmerie Royale. Mineralogy and Found 1991–2004 classification (Hasnaa Chennaoui Aoudjehane, UHAC; Albert Table 3 reports classification of 90 of the 125 meteorite Jambon, UPVI; Michèle Bourot Denise, MNHNP): LL6, Fa29 fragments recovered from the Frontier Mountain blue ice ±1 Fs25 ± 1, S3, W0. Specimens: type specimens, ~340 g, field (northern Victoria Land, Antarctica) by the Italian UHAC and 46 g, NAU; main mass, Oakes. Some other pieces Programma Nazionale delle Ricerche in Antartide (PNRA) are at CNRST. between 2003 December and 2004 January. Table 3 also lists 8 meteorites recovered from the same blue ice field by earlier Bukhara 39°46′47.2′′N, 64°36′01.3′′E PNRA/EUROMET expeditions which appeared in Grady Uzbekistan (2000) with incomplete classification. Mineralogy and Fall 2001 July 9, 4.00 hrs (or July 8, 23.00 UT) classification by A. Burroni and L. Folco (MNA-SI), P. (CV3) Rochette (CEREGE), A. M. Fioretti and R. Carampin, One stone, weighing 5.3 kg, fell in a field, 15 km away from (UPad), M. Macrì, A. Maras and M. Serracino (URoma). Bukhara city. A shepherd saw the fall and recovered the stone. Specimens: Main mass, type specimens and thin sections, Later his grandson learned about meteorites in school and MNA-SI. remembered about the stone. He thought that it might be a meteorite and reported about the stone to the Ulugh Beg Antarctic CAS Meteorites Astronomical Institute of the Uzbek Academy of Sciences. (51 meteorites) Shuhrat A. Ehgamberdiev of the Institute sent a sample of the Antarctica meteorite to the Vernadsky Institute in 2004. Mineralogy and Found 2002–2003 classification (M. A. Ivanova Vernad., F. Brandstätter NHMV). Table 4 reports classification of 50 meteorites collected in Fusion crust is well developed, dark grey. The meteorite Grove Mountains by the Polar Research Institute of China, consists of POP, PO, BO, and PP , Shanghai. Classification: B. Miao, Y. Lin, R. Lu and D. Wang, fragments, CAIs, and matrix. Matrix/chondrule ratio is 0.6; CAS; H. Wang, Y. Liang, R. Wang, J. Ji, W. Zhang and X. chondrule sizes vary from 0.2 to 2 mm, 0.6 mm on average. The Meteoritical Bulletin No. 89 A203

Chondrules of type I are most abundant. Minor phases are anonymous finder in the desert of . Classification plagioclase, nepheline, jadeite, (Ni 5.4 wt%, Co and mineralogy (A. Greshake and M. Kurz, MNB): contains 0.09 wt%), (up to 47 wt% Ni), sulfides, mostly . chondrules (mean diameter, 760 µm, abundance 25 vol%), Olivine, Fa0.9–60; Al2O3 0.2 wt%, Cr2O3 0.2 wt%, CaO CAIs, and mineral fragments set into a fine-grained matrix; 0.2 wt%, (mean values), pyroxenes are present as olivine, Fa19.6 (range 2.2–30.3), low-Ca pyroxene, Fs1.8– orthopyroxene, Fs1–11Wo0.6–3.6, Al2O3 up to 8 wt%, pigeonite, 7.2Wo0.6–1.3; oxygen isotopes (I. A. Franchi and R. C. 17 18 17 Fs1.7–11Wo5.2–11, Al2O3 up to 4 wt%; augite, Fs1.4–9Wo34–42, Greenwood, OU): δ O = –4.98‰, δ O = –1.71‰, and ∆ O = Al2O3 up to 12 wt%, and fassaite, Fs0.3–1.5Wo46–57, Al2O3 –4.09‰; low degree of shock; moderate degree of weathering. 17 wt%, TiO2 15 wt%. Petrological type 3; shock stage, S1; Specimens: main mass with anonymous finder; type specimen, weathering grade, W1. Specimens: type specimen, 320.3 g, 20.7 g MNB. and a thin section, Vernad; main mass with Sh. A. Ehgamberdiev in the Ulugh Beg Astronomical Institute of the Dhofar Meteorites Uzbec Academy of Sciences, Uzbekistan. Oman (67 meteorites) Capot Rey 20°07.556′N, 10°12.336′E Table 6 reports classifications of 51 meteorites from the Niger Dhofar region of Oman. Found 2004 March Ordinary chondrite (H5) Dhofar 744—Correction Many stony fragments totalling 38 kg were found by G. The find location for this sample is 19°15.6′N; 54°48.3′E Moreau in the erg Capot-Rey, Ténéré du Tafassasset, Niger. The stones define an elliptical measuring 7 × Dhofar 950 19°19.5′N, 54°46.9′E 3.5 km, with a NE-SW major axis. The largest fragment Oman weighs 2 kg. Mineralogy and classification: (E. Dransart, Found 2003 November 11 EMTT) Olivine: Fa18.1; low-Ca pyroxene Fs15.2; shock stage (feldspathic impact melt ) S2; weathering degree W1. Specimens: type specimen, A grey stone weighing 21.7 g was found in the Dhofar region 32.1 g, MNHNP, main mass with finder. of Oman. Mineralogy and classification (M. Nazarov, Vernad., Th. Ntaflos, University of Vienna): fusion crust is absent. The Cotopaxi 38°27.89′N, 105°42.09′W meteorite is an impact melt breccia with mineral fragments and Femont County, Colorado, USA lithic clasts cemented by a glassy impact melt matrix. The lithic Found 2000 October 8 clast population includes mainly granulitic rocks of Iron (ungrouped, IAB complex) anorthositic, troctolitic, gabbro-noritic and gabbro- Richard and Sharon Walker found a single mass of 243 g anorthositic compositions. The sample contains abundant while prospecting for gold samples on a forested hillside with veins of glass. Mineral compositions are as follows: feldspar, a metal detector. The meteorite was buried about 20 cm deep An92–98Or0–0.3; orthopyroxene, Wo0.4–5En55–91; clinopyroxene; in soil under a small tree and the mass was intergrown with Wo5–44En30–72; olivine, Fo52–92 (Fe/Mn ≈ 85 at); accessory the tree roots. Classification and analysis (J. Wasson, UCLA): phases are Al-rich enstatite, Mg, Al-rich spinel, pleonaste, Al- Metal composition determined by INAA is: Ni = 9.8 wt%, Co rich chromite, ilmenite (1.1–8.5 wt% MgO), armalcolite, = 0.50 wt%, Ga = 48 µm/g, As = 17 µg/g, Ir = 1.4 µg/g, Au = silica, troilite, and Fe-Ni metal (0.6–8 wt% Ni; 0.4–1.1 wt% 1.7 µg/g. The composition is unique compared to all other Co). Matrix glass composition (wt%): SiO2 43.9, TiO2 0.05, known meteorites. Cotopaxi is an ungrouped member of the Al2O3 33.1, FeO 1.08, MgO 1.77, CaO 18.6, Na2O 0.37. The IAB complex. Type specimens, 21.43 g, UCLA; 20.33 g, stone contains moderately weathered gypsum, celestite, and Fe Denver. Main mass (190 g), Denver. hydroxides. The meteorite may be paired with Dho 302, 303, 305, 306, 307, 309, 310, 311, 730, 731 found nearby. Dar al Gani Specimens: type specimens of 4.8 g and a thin section, Vernad. Libya The main mass is held by an anonymous finder. (5 meteorites) Table 1 reports classification of 5 meteorites found in the Dhofar 955 19°03.27′N, 54°45.23′E desert of Dar al Gani, Libya. Oman Found 2003 February 6 Dar al Gani 1040 27°16.88′N, 16°24.50′E Carbonaceous chondrite (CM2) Libya One fragment of an individual stone weighing 16 g was found Found 2001 May 21 on February 2003 in the Dhofar region of Oman. Mineralogy Carbonaceous chondrite (CV3) and classification (M. Ivanova, Vernad, F. Brandstätter, Fifteen stones totalling 781 g were found 2001 May 21 by an NHMV): fusion crust is dark brown, the meteorite consists of A204 S. S. Russell et al. altered POP, rare BO chondrules and their fragments, olivine stones may be paired. Specimens: type specimens of 4.8 g and aggregates sometimes with a halo around. Refractory a thin section on deposit at Vernad. The main mass is held by inclusions consist of perovskite, spinel, and hydrously altered an anonymous finder. silicates. Olivine, Fa0.5–35, CaO 0.24 wt%, Cr2O3 0.40 wt%. Pyroxene is rare, present as orthopyroxene, Fs1.4–5.6Wo0.8–2.4 Dhofar 979 19 45.4′N, 54 56.2′E and augite, Fs2.0Wo36.6. Minor phases are tochilinite, Oman kamacite, pyrrhotite, , Cr- and P-rich sulfides, Found 2004 chromite, escolaite, , and Ca carbonates. The Achondrite (ureilite) matrix is hydrously altered, and composed mainly of A completely fresh, crusted stone of 1063 g was found by phyllosilicates and rare isolated grains of olivine and Michael Farmer in the Dhofar region of Oman on January 8, pyroxene. Weathering grade is W1. Shock stage is S1. 2004. Description and classification (T. Bunch and J. Wittke, Specimens: type specimen, 4.3 g, and one polished section, NAU): medium-grained typical ureilite with abundant very Vernad; main mass with anonymous finder. fine-grained, wormy graphite at grain boundaries and included within olivine and pigeonite. Olivine cores, Fa16.5, Dhofar 960 19°23.8′N, 54°33.5′E FeO/MnO = 36 and rims, Fa15.8; pyroxene, Fs14.9Wo5.0. Very Oman little metal and terrestrial Fe oxides are present. Shock level, Found 2003 November 16 S1 and lightly weathered. Specimens: type specimen, 44.7 g, Lunar meteorite (feldspathic impact melt breccia) NAU: main mass, Farmer. A grey stone weighing 35.4 g was found in the Dhofar region of Oman. Mineralogy and classification (S. Demidova, Dhofar 1222 18°12.25′N, 54°03.40′E Vernad., F. Brandstätter, NHMV): Fusion crust is absent. The Oman meteorite is an impact melt breccia with abundant mineral Found 2003 fragments and lithic clasts set within a fine-grained impact () melt matrix. The lithic clasts are impact melt breccias and A single stone, weighing 93 g, was found by Labenne. granulitic rocks of anorthositic, gabbro-noritic, troctolitic, Classification and mineralogy (M. Bourot-Denise, MNHNP): and noritic compositions. The presence of VLT mare basalt has an equigranular texture with a mean grain size of about clasts, KREEPy and rare granitic fragments is a characteristic 200 µm. A few well-rounded chondrule relics are present. feature of the meteorite. Glass veins and fragments are Olivine, Fa6.8; pyroxene, Fs8.1; wide patches of , common. Mineral compositions are as follows; plagioclase, large euhedral chromites; Fe-Ni metal contains schreibersite An57–98Or0–6; orthopyroxene, Wo3–5En66–78; clinopyroxene; inclusions, troilite contains about 0.35 wt% Cr. Shock stage Wo5–43En0.4–73; olivine, Fo4–90 (Fe/Mn ≈92 at); accessory S2, weathering grade W2/3. Specimens: type specimen, 19 g, minerals are ulvöspinel, Cr-rich ulvöspinel, Ti-rich chromite, MNHNP; main mass with finders. Al-rich chromite, pleonaste, ilmenite (0.7–7.4 wt% MgO), silica, troilite, Fe-Ni metal (5–21 wt% Ni; 0.3–0.7 wt% Co); Dhofar 1224 19°19.605′N, 54°46.507′E K-Ba feldspar, pyroxferroite, whitlockite, apatite, Oman baddeleyite, Zr armalcolite and Zr-rich phases. The stone is Found 2003 September 28 moderately weathered; calcite, gypsum, celestite, smectite Lunar meteorite (feldspathic regolith breccia) and Fe hydroxides are present. The meteorite was found One 4.57 g stone, partly covered with fusion crust, was found close to Dho 925 and they are similar in texture, petrography by an anonymous prospector near the find locations of the and mineral chemistry. The stones may be paired. lunar meteorites Dho 081/280/910 and Dho 302/908/1085 on Specimens: type specimens of 7.4 g and 2 thin sections a desert plateau near Wadi Quitbit, Dhofar, Oman. It was deposited at Vernad. The main mass is held by an anonymous subsequently purchased by N. Classen. Classification and finder. mineralogy (A. Irving and S. Kuehner, UWS): glass-rich, melt-matrix highland regolith breccia containing sparse, Dhofar 961 19°23.9′N, 54°33.8′E small mineral and lithic clasts. Minerals include exsolved Oman pigeonite, augite (Fs21.4Wo38.3 to Fs24.1Wo35.0, FeO/MnO = Found 2003 November 12 54.5–60.7), orthopyroxene (Fs27.6Wo9.4 to Fs37.1Wo3.0, FeO/ Lunar meteorite (feldspathic impact melt breccia) MnO = 49.8–50.1), olivine (Fa27.3–46.7, FeO/MnO = 80–105), A grey stone weighing 21.6 g was found nearby to the Dho anorthite (An99.5–99.6), metal (10 wt% Ni and 40 wt% Ni), 925 and 960 lunar meteorites in the Dhofar region of Oman. ilmenite, Ti-Al-bearing chromite and troilite. The largest Mineralogy and classification (S. Demidova, Vernad, F. lithic clast is a troctolite composed of Brandstätter, NHMV): the meteorite is similar to Dho 925 and olivine+anorthite+ilmenite. This specimen is probably paired 960 in texture, mineralogy and mineral chemistry and the to Dho 081, Dho 280 and Dho 910 found nearby. Specimens: The Meteoritical Bulletin No. 89 A205

type specimen, 1.19 g, and one polished thin section, UWS; olivine (Fo85–88,CaO 0.1 wt%), low-Ca pyroxene (En68–71 main mass, Classen. Wo13–8) and skeletal Ca-rich pyroxene in a feldspathic Fe-rich glass. Two very fine-grained dark clasts, about 2 mm in size, Dhofar 1275 18°49.711′N, 54°38.374′E are similar to matrix of carbonaceous chondrites, containing Oman both Mg-rich and Fe-rich hydrous minerals. Kamacite and Found 2003 February 6 troilite are present as minor phases in the breccia. Carbon-rich Ordinary chondrite (L7) veins and pockets are common. Diamond, positively One stone weighing 499 g was found on February 2003 in the identified on the basis of its cathodoluminescence, constitutes Dhofar region of Oman. Mineralogy and classification (M. abundant small grains only within carbonaceous areas. Ivanova, Vernad) fusion crust is dark brown, chondrules are Graphite lamellae, generally deformed, are completely devoid not defined, matrix is coarse-grained. Olivine, Fa24.8, of diamond. Shock deformation is high and varies in different orthopyroxene, Fs21.1Wo3.6 CaO >1.57 wt%. Plagioclase clasts. Weathering is minor. Specimens: main mass, 2.82 g, grains are up to 200 µm. Weathering grade is W4. Shock stage one thin section, MNA-SI, one thin section, OU. is S2. Specimens: type specimen, 59 g, and one polished section, Vernad; main mass with anonymous finder. Frontier Mountain 90233 72°57′22′′S, 160°26′18′′E Antarctica Fountain Hills 33.61°N, 111.72°W Found 1991 January 10 Maricopa County, Arizona, USA Achondrite (monomict ureilite) Found 2002 October 5 A 31.89 g stony fragment was found by a PNRA/EUROMET Carbonaceous chondrite (Bencubbin-like meteorite) team on the Frontier Mountain blue ice field. Mineralogy and A single stone weighing 60 g was found by a hiker on a desert classification (A. M. Fioretti and R. Carampin, UPad): FRO trail near his home in Fountain Hills, AZ. Classification and 90233 is a relatively coarse-grained (grain size up to 2 mm) analysis (D. Lauretta, A. R. La Blue, UAriz; M. Killgore, monomict ureilite composed of 76% olivine, 16% low-Ca SML): The stone is a CB carbonaceous chondrite, no obvious pyroxene and 8% interstitial graphite. Olivine has Fo77 shock features, weathering grade W1. The meteorite contains average core composition (range Fo75.4–78.5) and Fo90.5 abundant, large (diameter up to 4.3 mm), volatile-depleted, reduced portions. Pyroxenes typically occur as mosaicized, barred olivine, porphyritic, and granular chondrules, no fine- turbid, twinned crystals with En76Wo4.7 composition. Graphite grained matrix, and ~25% modal abundance of metal, lower forms intergranular flakes up to 1 mm in size. The shock stage than for other Bencubbin-like meteorites. Metal occurs is S4. Weathering is minor. Specimens: main mass, 22.6 g, one almost exclusively outside of chondrules. Olivine, Fo96–98; thin section, MNA-SI; 8.79 g and one thin section, OU. low-Ca pyroxene, En96, Fe/Mn = 23, 1.7–1.9 wt% CaO; plagioclase, An99, 1.0 wt% MgO, 0.4 wt% FeO. Metal Frontier Mountain 93001 72°57′20′′S, 160°29′29′′E composition is 6.3–6.8 wt% Ni, 0.17–0.36 wt% Co, single Antarctica grains are unzoned. No sulfides have been found. Oxygen Found 1994 January 4 isotopic composition: δ17O = –1.45‰, δ18O = +1.28‰. Primitive achondrite (acapulcoite-) Nitrogen isotopic composition: δ15N = +48‰; see Lauretta et This 4.84 g small stone is a fragment ~16 × 13 × 12 mm, al. (2004), Blue et al. (2004). Specimens: type specimen, 12 g, angular, 20% fusion-crusted, found by a PNRA/EUROMET UAriz; Main mass, SML. team. Mineralogy and classification (A. Burroni and L. Folco, MNA-SI): FRO 93001 is a medium-grained to coarse-grained, Frontier Mountain 90200 72°57′20′′S, 160°32′16′′E gabbroic rock consisting of (in order of abundance) Antarctica orthoenstatite (Fs13.3 ± 0.4Wo3.1 ± 0.2), oligoclase Found 1991 January 10 (Ab80.5 ± 3.3Or3.2 ± 0.6), augite (Fs6.1 ± 0.7Wo42.3 ± 0.9) and traces of Achondrite (polymict ureilite) olivine (Fa13.3 ± 0.3; Mn/Mg = 0.006). Corroded xenoliths of A 3.19 g stony fragment was found by a PNRA/EUROMET probable lodranitic composition float in the gabbroic host team on the Frontier Mountain blue ice field. Mineralogy and lithology; they mainly include granoblastic olivine Fo90.4 ± 0.7 classification (A. M. Fioretti and R. Carampin, UPad): FRO with average grain size of 400 µm, lesser Fe-Ni metal, and 90200 is a polymict ureilite breccia. Lithic fragments are minor chromite (Cr/(Cr+Al) = 0.84; Fe/(Fe+Mg) = 0.64), <2 mm in size and appear oriented. Olivine in ureilite clasts phosphates, schreibersite, and troilite. The rock (including ranges from Fo75 to Fo92 shows highly reduced rims (up to xenoliths) is devoid of shock features (S1) and nearly Fo94) and have CaO = 0.35 wt% mean content. Low-Ca unweathered (W1). FRO 93001 is similar to the igneous pyroxene ranges Wo0.5–14En54–94. Augite is only found as lithology that intrudes an acapulcoite host in the Lewis Cliff isolated crystals. Individual plagioclase crystals range from (LEW) 86220 meteorite described by McCoy et al. (1997). albitic (Ab91.3An0.3Or8.4) to anorthitic (Ab4.5An95.5) Specimens: main mass, 2.57 g, two thin sections, MNA-SI; one composition. One igneous-textured clast consists of euhedral thin section, NHM, type specimen, 1.60 g, OU. A206 S. S. Russell et al.

Frontier Mountain 03005 72°57′18.5′′S, 160°23′03.3′′E meteorites include 1 , 1 , 3 , Antarctica 7 carbonaceous chondrites, and 39 ordinary chondrites. Found 2004 January 1 Specimens: main mass, type specimens and thin sections at (EL4) the Polar Research Institute of China (PRIC). A complete, fusion-crusted stone weighing 20.66 g was found by a PNRA team on the Frontier Mountain blue ice field. Grove Mountains 020005 73°05′51′′S, 75°12′17′′E Mineralogy and classification (A. Burroni and L. Folco, Antarctica MNA-SI): chondrules are readily delineated with mean Found 2002 diameter of 670 µm; enstatite is commonly monoclinic and Carbonaceous chondrite (CM2) has homogeneous composition Fs0.8Wo0.4; traces of olivine, The stone weighs only 0.38 g, and has an irregular shape, Fa0.1 are present. Opaque minerals include troilite, kamacite partially covered by brownish-black fusion crust. (Ni = 6.13, Si = 0.67 wt%), schreibersite and alabandite (Mn Classification and mineralogy (NU): Chondrules are small = 76.8, Fe = 20.1 and Mg = 3.05 wt%). Shock stage is S1, (0.1–0.5 mm in diameter), and less abundant than the opaque weathering grade is W1. Specimens: main mass and one thin matrix (chondrule/matrix ratio of ~35/65). Aqueous alteration section, MNA-SI. products are abundant. Accessory minerals are sulfide and metallic Fe-Ni (<1 vol%). A few Ca-Al-rich inclusions were Frontier Mountain 03022 72°57′03.2′′S, 160°27′16.5′′E found. Shock stage is S1; weathering grade is W1. Antarctica Found 2003 December 29 Grove Mountains 020015 73°07′17′′S, 75°06′23′′E Achondrite (polymict ureilite) Antarctica A stony fragment weighing 2.47 g was found by a PNRA Found 2002 team on the Frontier Mountain blue ice field. Mineralogy and Carbonaceous chondrite (CK4) classification (A. M. Fioretti and R. Carampin, UPad): The stone is a small (10.1 g), dark grey and friable fragment polymict ureilite breccia containing a wide variety of mineral partially covered with a black fusion crust. Classification and and lithic clasts <2 mm in size. Typical ureilite clasts show mineralogy (CAS): There are abundant mineral fragments and equilibrated texture with triple junctions, inter-granular several lithic clasts, with a few large chondrules (0.5–1.5 mm lamellae of graphite, and olivine cores ranging from Fo75 to in diameter). The matrix (~60 vol%) is recrystallized Fo87 with highly reduced rims (up to Fo93). Most isolated (<10 µm); metal and sulfide are common (a total of ~5% olivine crystals show the same compositional range. Low-Ca vol%), as opaque nodules and tiny grains in chondrules and pyroxene in lithic clasts and isolated crystals shows a wide matrix. Olivine (Fa30.2±0.4) and low-Ca pyroxene (Fs20.7 ± 9.8) compositional range, En67–99Wo0.2–12. Rare augite is found as are FeO-rich. Shock stage, S1; weathering grade, W1. isolated crystals. Individual plagioclase crystals are mainly albitic, Ab94.7Or7.14. Interstitial glass has high SiO2 content Grove Mountains 020017 73°05′47′′S, 75°11′03′′E (up to 75 wt%). The breccia contains five very fine-grained Antarctica dark clasts, up to 1.8 mm in size, similar carbonaceous Found 2002 chondrite matrix material. The clasts are almost opaque and Carbonaceous chondrite (CM2) contain both Mg-rich and Fe-rich, very fine-grained hydrous A black fragment (2.2 g) contains light grey chondrules and minerals. Opaque mineral include abundant troilite and minor inclusions on the surface. Classification and mineralogy kamacite, schreibersite. Shock varies in the different clasts up (CAS): Chondrules and fragments are small (50–300 µm in to shock stage S5. Weathering is minor, W1. Specimens, main diameter), and less abundant than the opaque matrix. Several mass, MNA-SI. Ca-Al-rich inclusions and amoeboid olivine aggregates were found. Phyllosilicate is common in the matrix. Olivine Grove Mountains (GRV) 73°05′S, 75°12′E (Fa9.8 ± 13) and low-Ca pyroxene (Fs2.0 ± 3.4) are highly (51 meteorites) heterogeneous, showing compositional zoning on Antarctica backscattered electron images. Shock stage, S1; weathering Found 2002–2003 grade, W1. Table 4 summarizes classification of 51 of 4448 meteorites recovered from Grove Mountains, Antarctica, by the 19th Grove Mountains 020025 73°04′39′′S, 75°16′31′′E Chinese Research Expedition (CHINARE) from 2002 Antarctica December to 2003 February. Thirty-eight of these Found 2002 representative samples were analyzed by CAS (B. Miao, Y. Carbonaceous chondrite (CM2) Lin, R. Lu and D. Wang from Chinese Academy of Sciences), A partially crusted fragment of 3.55 g was found. and the other 13 meteorites were determined by NU (H. Classification and mineralogy (CAS): Chondrules are small Wang, Y. Liang, R. Wang, J. Ji, W. Zhang and X. Chen). The (<500 µm, most 100–300 µm in diameter), and less abundant The Meteoritical Bulletin No. 89 A207

(26 vol%) than the opaque matrix (~70 vol%). Other (En74.5 ± 0.3Wo8.0 ± 0.2Fs17.5 ± 0.2) and olivine cores (Fo79.6 ± 0.2) components are many mineral fragments, less abundant Ca- are homogeneous. All grains of olivine have FeO-poor rims Al-rich inclusions and amoeboid olivine aggregates, and rare (Fa as low as 6.4 mol%), which contain abundant fine-grained metallic Fe-Ni and sulfides. Phyllosilicates are very common. inclusions of Ni-poor metal and sulfide. The carbonaceous All Ca-Al-rich inclusions are strongly altered. Olivine matrix is composed of two distinct assemblages, i.e., most (Fa10.2 ± 16) and low-Ca pyroxene (Fs1.8 ± 1.1) are highly abundant fine-grained mixtures of forsterite, enstatite, Ni- heterogeneous. Shock stage, S1; weathering grade, W1. poor metal and sulfides, and less abundant diamond-bearing graphite patches or veins. The presence of diamond was Grove Mountains 020090 72°59′58′′S, 75°15′40′′E confirmed by Raman spectrum and CL analyses. Limonite Antarctica veins are common. Shock stage, S2/S3; weathering grade, Found 2003 W3. Martian meteorite (lherzolite) This stone weighs 7.54 g, and measures 24 mm × 22 mm × Grove Mountains 021579 72°57′55′′S, 75°12′55′′E 20 mm in size. It has a nearly complete glossy fusion crust with Antarctica clearly visible flow lines. Classification and mineralogy Found 2003 (CAS): It consists of poikilitic and interstitial parts. The Carbonaceous chondrite (CO3) poikilitic part is composed of several pyroxene oikocrysts, The fragment weighs 6.57 g, with a few remains of fusion each having a pigeonite core and a thick augite rim and, crust. Classification and mineralogy (CAS): Chondrules are enclosing several euhedral grains of olivine and chromite. The small and have a bimodal size distribution, with one peak at interstitial part consists of olivine and pigeonite and 30–100 µm and the other at 350–600 µm in diameter. Modal , with accessory laths of merrillite coexisting with abundance ratio of chondrule to opaque matrix is 1.2. Fe-Ni maskelynite. Magma inclusions occur mainly in olivine and a metal and sulfide are rare. Ca-Al-rich inclusions were found, few exist in pyroxene oikocrysts. Mineral chemistry: olivine, and they are strongly altered. Silicates are highly Fa30–40; pigeonite, En60–72Fs24–29Wo3–14; augite, En47–52Fs16– heterogeneous: olivine, Fa18.8 ± 20; low-Ca pyroxene, Fs7.0 ± 12. 19Wo31–36; maskelynite, An37–57Ab41–58Or1–6; MnO/FeO ratio Shock stage, S1; weathering grade, W1. of pyroxenes, 26.4. Shock stage, S5; weathering grade, W1. This meteorite is unlikely to be paired with GRV 99027, Grove Mountains 021710 72°47′25′′S, 75°17′36′′E another Martian lherzolite found in the same region, based on Antarctica their distinct petrographical and mineral chemical features. Found 2003 Carbonaceous chondrite (CR2) Grove Mountains 020099 72°59′51′′S, 75°12′15′′E This black stone weighs 442.6 g. It is heavily fractured, with Antarctica a portion covered with fusion crust. Classification and Found 2003 mineralogy (CAS): There are abundant large (1–4 mm in Pallasite diameter), multi-layered and metal-rich type I chondrules, This meteorite weighs 23.5 g, and has an irregular shape and a few type II chondrules. A spinel-rich inclusion (380 × without any fusion crust. Large greenish crystals of olivine 680 µm in diameter) was found. Metallic Fe-Ni is abundant appear on the surface. Classification and mineralogy (CAS): It (5.9 vol%), and occurs predominantly inside chondrules. consists of metallic Fe-Ni and olivine in nearly equal Silicates are FeO-poor: olivine, Fa1.4 ± 0.6, low-Ca pyroxene, proportions. The metal shows a Widmanstätten pattern with Fs2.1 ± 0.6. Accessory phases are phyllosilicates, sulfides and ~25 µm kamacite bandwidths. Olivine is 0.5–1.2 mm in size. magnetite. Shock stage, S1; weathering grade, W1. Mineral chemistry: kamacite, 4.72–5.64 wt% Ni, 0.63– 0.79 wt% Co; taenite, 9.19–48.7 wt% Ni, 0.18–0.68 wt% Co; Grove Mountains 021788 72°46′24′′S, 75°19′20′′E olivine, Fa11.2 ± 0.1. Antarctica Found 2003 Grove Mountains 021512 72°56′06′′S, 75°19′07′′E Achondrite (ureilite) Antarctica This meteorite weighs 24.9 g, and is somewhat cone-shaped. Found 2003 The surface is partially covered with black fusion crust. Achondrite (ureilite) Classification and mineralogy (NU): it consists mainly of The 143.4 g meteorite is hemispherical in shape, and most of coarse-grained (0.5–2.0 mm) silicates (~70 vol%) embedded the surface is covered with black fusion crust. Classification in fine-grained carbonaceous matrix. Modal abundances: and mineralogy (CAS): It consists mainly of subhedral to olivine 45 vol%, pyroxene 50 vol%, carbonaceous matrix anhedral olivine (up to 1.0–3.5 mm in size) and a few grains <5 vol%. Pyroxene (Fs22.6) and the core of olivine (Fa22.3) are of pigeonite embedded in carbonaceous matrix. Some grains homogeneous. However, olivine is characterized by of olivine have 120° triple junctions. Pigeonite occurrence of reduced zones (~100 µm wide, Fa1.5) along its A208 S. S. Russell et al. embayed boundaries and cracks. Abundant tiny metallic Fe and matrix lumps. Fe-Ni metal comprises from 50 to 70 vol%, (<1 vol%) is enclosed in the reduced zones and in the C-rich and contains 4.2–8.4 wt% Ni, 0.2–0.5 wt% Co, and 0.03– matrix. The coarse-grained olivines show triple junctions. 0.6 wt% Cr; Co/Ni ratio is approximately solar. Chondrules Shock stage is S3; weathering grade is W3. do not contain any Fe-Ni metal grains, they are Mg-rich, and consist of pyroxene-rich cryptocrystalline material. Olivine, Grove Mountains 022459 72°46′26′′S, 75°19′37′′E Fa2.5, rare FeO-rich olivines, Fa10–38; pyroxene, Fs2.1Wo1.7, Antarctica FeO-rich pyroxene, Fs8–12Wo0.8–1.8; troilite is Cr-rich, Found 2003 2.5 wt% Cr. INAA data for a 20 mg chip: 2.74 wt% Ni; Carbonaceous chondrite (CV3) 717 ppm Co; 2608 ppm Cr, 8.2 ppm Sc, and 1.59 ppm Ir. This is a small (1.1 g) dark grey fragment, with a little Petrological type 3; shock stage, S1; weathering grade, W1. remaining black fusion crust. White Ca-Al-rich inclusions Specimens: type specimen, 24.3 g, and two sections, Vernad; and light grey amoeboid olivine aggregates (AOAs) appear main mass with anonymous finder. on the broken surface. Mineralogy and classification (CAS): the sizes of chondrules range from 0.6–2.0 mm. Modal Jiddat al Harasis 054 19°37.82′N, 55°06.91′E abundance ratio of chondrules plus amoeboid olivine Oman aggregates to matrix is ~1. Olivine, Fa7.0 ± 5.5; low-Ca Found 2004 January 15 pyroxene, Fs1.6 ± 0.7. Metallic Fe-Ni is rare. Shock stage, S1; Achondrite (ureilite) weathering degree, W1. Fifty-two pieces of meteorite with total weight of 5079 g were found on January 2004 in the desert of Oman. Fusion crust is Grove Mountains 022931 72°46′28′′S, 75°19′11′′E dark brown and partly preserved. Mineralogy and Antarctica classification (C. Lorenz, Vernad; F. Brandstätter, NHMV): Found 2003 the rock has medium- to coarse-grained granular Achondrite (ureilite) metamorphic texture. Few large inclusions of silicates are This is a fragment (1.24 g) without any fusion crust. presented in the groundmass. Main phases are olivine (Fo86; Classification and mineralogy (CAS): the meteorite has a 0.2–0.7 wt% Cr2O3, 0.18 wt% CaO) and pigeonite En83Wo5 cataclastic porphyritic texture, consisting of coarse-grained (0.9–1.2 wt% Cr2O3). Large grains of pyroxene contain of olivine (19.1 vol%) and pigeonite (14.1 vol%) embedded in feldspathic glass inclusions (Ab58An40) and minor augite fine-grained carbonaceous matrix (66.3 vol%). The olivine (En59Wo31). Accessories are chromite, Fe metal, Ni-Cr-rich grains have embayed boundaries, and show significantly troilite (3.9–6.7 wt% Ni; 6.7–7.3 wt% Cr) and Ni-poor troilite reduced features with FeO-poor rims (Fa as low as 7 mol%). (0.7 wt% Ni; 4.1 wt% Cr). Troilite and orthopyroxene form The reduced rims contain abundant tiny inclusions of Ni-poor the fine-grained intergrowth within olivine along thin metal and sulfides. The pigeonite (En71.7 ± 0.3Wo10.4 ± fractures, filled by iron hydroxides with troilite relics. 0.2Fs17.9 ± 0.2) and the core of olivine (Fa21.2 ± 0.3) are rather Aggregates, 100–800 µm in size, composed by graphite and homogeneous. The carbonaceous matrix consists diamond grains, occur between silicate grains. Total amount predominantly of fine-grained mixtures of forsterite, of carbon material is 2.8 vol%. Silicates have thin MgO-rich enstatite, Ni-poor metal and sulfides, with a few diamond- rims with tiny metal inclusions along the margins of graphite- bearing graphite patches. The occurrence of diamond in diamond assemblies. Specimens: type specimen, 640 g, one graphite patches was confirmed by the Raman spectrum and thin and two polished sections, Vernad; main mass with cathodoluminescence. The sample contains many veins of anonymous finder. limonite, and appears dark brown in color. Weathering grade, W3; shock stage, S2/S3. Kalahari 008 20.9818°S, 22.9766°E Kalahari, Botswana Isheyevo ~53°37′N, 56°20′E Found 1999 September Bashkortostan, Russia Lunar meteorite (feldspathic regolith breccia) Found 2003 October A single stone of 598 g was found in September 1999 by an Carbonaceous chondrite (Bencubbin-like meteorite) anonymous finder in front of a sand dune within the Kalahari One stone, weighing 16 kg, was found by a tractor driver in a desert. The rock is an anorthositic breccia having typical field during harvest carrying in the Ishimbai region of clasts of lunar highland breccias (e.g., feldspathic crystalline Bashkortostan, close to the Isheyevo village. A small piece of melt breccias, granulitic lithologies, cataclastic anorthosites, the meteorite was issued to the Vernadsky Institute by etc.) embedded within a well-lithified matrix. An impact melt Kazakov D.A. and Polozkov A.G. September 2004. spherule indicates that this rock derives from the regolith. The Mineralogy and classification (Ivanova, Vernad, Ulianov, regolith origin is also supported by the finding of solar wind MSU): fusion crust is well developed, dark brown. The implanted rare gases (L. Schultz, Mainz). Classification and meteorite consists of Fe-Ni metal grains, C, POP, rare BO mineralogy (Anna Sokol and Addi Bischoff, Mün): olivine, chondrules (0.02–1 mm in size), chondrule fragments, CAIs, Fa63 ± 18; pyroxene, Fs42 ± 10; plagioclase, An85–98. The shock The Meteoritical Bulletin No. 89 A209 stage of the rock is S4, the weathering grade is W1. Oxygen 17.7 and 23.8 (n = 6) with an average of 20.9. Fs content in opx isotopic composition: δ18O = +6.52‰; δ17O = +3.32‰; ∆17O varies from 8.5 to 31.5 (n = 7) with an average of 20. Shock = –0.07‰ (R. N. Clayton, UChi); concentrations of selected stage, S2. Specimens: the single stone is at GSI, Kolkata. elements (XRF or INAA; H. Palme, G. Weckwerth, Köln) in wt%: Al: 14.68; Si: 20.73; Mg: 2.68; Fe: 3.5; Ca: 11.1. Kidairat—Reclassification Specimen: Type specimen, 20 g and polished thin section, This meteorite was first announced in The Meteoritical Mün; main mass, anonymous finder. Bulletin, No. 70. Mineralogy and reclassification (Yassir A. Abdu, Uppsala): the meteorite is homogenous, highly Kalahari 009 20.9818°S, 22.9766°E recrystallized (plagioclase grain size 50–100 µm) suggesting Kalahari, Botswana it is an H6 chondrite, Fa19, Fs16. Found 1999 September Lunar meteorite (basaltic fragmental breccia) Koltsovo 54°45.03′N, 36°58.68′E A single stone of about 13.5 kg was found in September 1999 Kaluga district, Russia by an anonymous finder in front of a sand dune within the Found 2004 July Kalahari desert, roughly 50 m apart from Kalahari 008. The Ordinary chondrite (H4) rock is different from the Kalahari 008 anorthositic breccia. It One stone weighing 20.02 kg was found by Svetlana has a heavily-brecciated texture and is basaltic in Murashova and Stanislav Murashov while collecting composition. The sample does not contain solar wind mushrooms 2 km SSW of the Koltsovo village. The stone was implanted rare gases (L. Schultz, Mainz). Classification and located at the edge of a ploughed field and was probably mineralogy (Anna Sokol and Addi Bischoff, Mün): olivine, removed there during cultivation. No other meteorite Fa50–99.9 (mostly Fa80–95); pyroxene is highly variable (Fs22–67 fragments were found in the field by Dr. Andrei Stanyukovich En10–64Wo6–41); plagioclase An86–96 (very few plagioclase of Moscow. Classification and mineralogy (M. Nazarov, have more albitic composition, An70–80). The shock stage of Vernad): chondrules of different types and their fragments are the rock is S4; the weathering grade is W1; however, calcite well defined; olivine, Fa20.0, PMD 2.7%; pyroxene shows 18 veins are present. Oxygen isotopic composition: δ O = variable composition, Fs5–24Wo0.2–7.2, the mean, Fs12.9Wo1.2; +6.87‰; δ17O = +3.45‰ (R. N. Clayton, UChi); shock stage S1; weathering grade W1. Specimens: 2034 g and concentrations of selected elements (XRF or INAA; H. a thin section, Vernad; main mass with the finders. Palme, G. Weckwerth, Köln; Münker, Mün) in wt%: Al: 6.76; Mg: 5.14; Fe: 12.47; Ca: 7.66. Zr/Hf = 30.2 and Nd/Ta= 17.4. Maigatari-Danduma ~12°50′N, ~9°23′E Specimens: type specimen, 20 g and polished thin section, Niger-Nigeria border Mün; main mass, anonymous finder. Fell 2004 August 1, 12:30 L.T. Ordinary chondrite (H5/6) Kasauli 29°35′N, 77°35′E A meteorite broke into pieces and fell across the Niger- Uttar Pradesh, India Nigeria border. One stone fell at the border town, Rigar Jobi Fell 2003 November 2, 17:00 IST in Maigatari Local Government Council, Nigeria. Mr. Malam Ordinary chondrite (H4) Musa was standing in front of his hut when he heard a strange A single stone weighing 16.82 kg accompanied by a sound like the sound of a plane coming towards him. When he thundering sound fell at Kasauli village, Muzaffarnagar looked at the sky, he saw a black object falling towards him. district, Uttar Pradesh, India creating an oval shaped crater. The object fell about 15 m away from him. His son, standing The fall was witnessed by villagers of Kasauli. The meteorite under a tree about 30 m away, also saw the falling object and was retrieved by the Geological Survey of India (GSI). The started running towards his father, but before he could reach single mass of Kasauli meteorite is almost an oriented one and him, the object had made it to Earth with a loud crash. Then has a plano-convex turtle-back shape with a truncated there was another loud fall about 2–2.5 km away, in ellipsoidal outline. The crust is greyish in color, netted in Danduma, a small village west-northwest of the town Adara nature. A few visible chondrules are distinct on the surface. on the Republic of Niger side, where two pieces of the Minute shiny metallic knobs are observed on the surface of the meteorite, including the main mass, were recovered. meteorite. Classification (B. K. Chattopadhyay and A. P. Neighbors running to the site found a black stone that had Thapliyal, GSI): the meteorite is essentially composed of shattered (or perhaps they broke it) into pieces. They brought olivine, pyroxene, abundant Fe-Ni metal, troilite, and some of the pieces to the local chief who presented them to devitrified glass. Olivine occurs in higher abundance than the emir of Maigatari Local Government Council, Jigawa pyroxene. A variety of well-defined chondrules of varying State, Nigeria. The total mass recovered was about 4.6 kg. shape and sizes (from 0.1 mm to 0.6 mm) are present. The Mineralogy and classification (F. Brandstätter, NHMV): H5/6 chondrule-matrix boundary is sharp. The matrix is fine- (Fa20.3, Fs18), S3, W0. Specimens: type specimen, 47 g, grained, recrystallized. Fa content in olivine varies between NHMV, main mass with anonymous purchaser. A210 S. S. Russell et al.

Neuschwanstein—Additional Information Northwest Africa 1052 This was reported in The Meteoritical Bulletin, Morocco No. 87. Two further stones of this EL6 chondrite fall have Found 2001 been recovered; a 2840 g stone recovered in Tyrol, Austria Acapulcoite approximately 1.5 km SE from the original fall, and a 1625 g A stone of 22 g was bought in Erfoud (Morocco) by Matteo piece found in Germany, approximately 1 km N of the Chinellato. Classification and mineralogy (G. Pratesi, V. original fall, at 10°48′29.4′′E, 47°32′01.9′′N. See Oberst et al. Moggi-Cecchi, L. Mancini, MSP; G. Sighinolfi and S. Lugli, (2004) for details. UMo): both thin section and type specimen sample look to be a fine-grained aggregate. In thin section it displays a granular Northeast Africa 001 texture with grains mainly of olivine, pyroxene, Fe-Ni alloy Sudan and troilite and ranging from 200 to 700 µm in dimensions. Found 2002 April Olivine is homogeneous and has a typical forsteritic Lunar meteorite (anorthositic regolith breccia) composition, (Fa5.95); orthopyroxene Fs7.6Wo1.4. High Ca- A brownish-grey stone weighing 262 g was found by a pyroxene (Fs3.6En51.1Wo45.3, Al = 1.44 mol%) and plagioclase prospector in northern Sudan near the Libya/Egypt/Sudan (An13.7Ab79.9Or6.4) are also common. Apart from silicates, border in 2002 April. Fusion crust is absent, fresh surface is major phases are metal and troilite. Accessory phases include grey to dark grey, and terrestrial alteration products are Na and Ca merrillite and magnesiochromite (Cr/(Cr+Al) = present at the meteorite edges and in penetrating cracks and 0.91; Fe:Mn:Mg ratios = 0.58:0.09:0.33). This meteorite veins. Classification and mineralogy (J. Haloda and P. shows a recrystallization texture with abundant 120° triple Tycova, PCU): a clast-rich anorthositic regolith breccia junctions and many interstices filled with metal. Based on containing numerous mineral fragments and lithic clasts texture (fine-grained), mineralogy, and chemistry (Cr content embedded in a well-consolidated microcrystalline impact of diopside varying from 1.18 to 1.43 wt%), the meteorite is melt matrix. Lithic clasts (up to 1 cm in size) are mainly of classified as an acapulcoite. Terrestrial weathering grade is anorthositic lithologies; impact-melt breccias of anorthositic rather low (W1); optical features (sharp extinction of olivine) composition are abundant and show commonly breccia-in- indicate that the sample is very weakly or not shocked (S1). breccia textures. Fragments of primary igneous rocks of Specimens: main mass with buyer (Matteo Chinellato); type anorthositic to gabbroic composition are common, containing specimen (4.7 g) and thin section, MSP. plagioclase, An95.1–97.2, low-Ca pyroxene, En46–65Wo2.1–5, high-Ca pyroxene, En35–48Wo37–44 and rare olivine, Fo79.4. Northwest Africa 1054 Sparse clasts of mare basalts (consisting of pigeonite plus Morocco anorthite plus accessory ilmenite), glass fragments, and Found 2001 spherules are present. Mineral fragments are of various Acapulcoite composition: feldspar, An92–99; orthopyroxene, Wo2–4En49–80; A stone of 86 g was bought in Erfoud (Morocco) by an clinopyroxene, Wo9–39En50–87; olivine, Fo48–82 (Fe/Mn 93– anonymous dealer. Classification and mineralogy (G. Pratesi, 100 atom%); accessory minerals are Mg-Al spinel, chromite, V. Moggi-Cecchi, L. Mancini, MSP; G. Sighinolfi and S. ilmenite (2–5 wt% MgO), troilite, Fe-Ni metal and silica. Lugli, UMo): composed of a fine-grained aggregate. In thin Several pyroxene grains have marginal symplectitic section it displays a granular texture with grains mainly intergrowths of fayalite plus hedenbergite plus silica after represented by olivine, pyroxene, Fe-Ni alloy and troilite and former pyroxferroite. Composition of the impact-melt matrix ranging from 200 to 700 µm in dimensions. Olivine is is (wt%): SiO2 = 45.7, Al2O3 = 24.1, FeO = 7.2, MgO = 7.4, homogeneous and has a typical forsteritic composition, CaO = 14.6, Na2O = 0.5, TiO2 = 0.5. Secondary calcite, (Fa6.37); orthopyroxene is bronzitic (Fs7.77Wo1.32). High-Ca barite, gypsum and Fe hydroxides occur in cracks. pyroxene (En51.23Fs3.33Wo45.44; Al = 1.50 mol%) and Specimens: type specimen, 20 g, and one polished thin plagioclase (An14.27Ab79.47Or6.25) are also common. Apart section, PCU; 5.8 g, and one polished thin section, UWS; from silicates, major phases are metal and troilite. Accessory 59.66 g, ROM; 60 g, Hupé; 9.7 g, Gregory; main mass with phases include Na merrillite and magnesiochromite (Cr/ finder. (Cr+Al) = 0.96; Fe:Mn:Mg ratios = 0.60:0.12:0.28). This meteorite shows a recrystallization texture with abundant Northwest Africa 120° triple junctions and many interstices filled with metal. Morocco, Western Sahara and Algeria Based on texture (fine grained), mineralogy, and chemistry (485 meteorites) (Cr content of diopside varying from 1.17 to 1.35 wt%), the Table 7 lists classifications for 485 meteorites found at meteorite is classified as an acapulcoite. Terrestrial unknown locations in Northwest Africa. weathering grade is rather low (W1); optical features (sharp The Meteoritical Bulletin No. 89 A211 extinction of olivine) indicate that the sample is very weakly equigranular (~1 mm grain size) crystals; no relict or not shocked (S1). The meteorite may be paired with NWA chondrules; prominent twinning in plagioclase. Mineral 1052. Specimens: main mass with buyer; type specimen modes: orthopyroxene, 37 vol%; olivine, 35%; plagioclase, (17.9 g) and thin section, MSP. 12%; Ca-rich pyroxene, 6%; troilite, 4.5%; metal (taenite only), 3.5%; chromite, 2%. Very homogeneous; silicate Northwest Africa 1628 compositional range is within the analytical precision of Northwest Africa ±0.2 mol%. Orthopyroxene, Fs19.1Wo1.3, Fe/Mn = 41; olivine, Found 2003 Fa22.0, Fe/Mn = 63 plagioclase, An53.4Or2.2; clinopyroxene, Carbonaceous chondrite (CK) Fs7.2Wo47; taenite, Ni = 16.7 wt%; chromite, Cr/(Cr+Al) = A 35.7 g stone was purchased in Rissani, Morocco in 0.73. Shock level, S1; weathering grade is W2. Specimens: September 2003. Description and classification (T. Bunch and 20.1 g, NAU; main mass, Oakes. J. Wittke, NAU): partially shock-melted/crystallized CK (S3- 6) of undeterminable petrologic grade. Cataclastic matrix Northwest Africa 1840 consists of a massive network of small-grained olivine (Fa31) Morocco with many micron-size magnetite inclusions (Cr2O3, Found 2003 0.57 wt%; Al2O3, 3.1 wt%) and plagioclase (An29.3). Several Enstatite achondrite (ungrouped) chondrules with thick, fine-grained rims, are mantled with A 132.8 g complete and partially crusted stone was purchased quench-form alumina-rich (5.6 wt%) low-Ca pyroxene in Erfoud, Morocco in August 2003. Description and (Fs23.2En76.8) set in Ca-rich mesostasis. Many other classification (T. Bunch and J. Wittke, NAU): the meteorite chondrules also show characteristics of partial melting. has an igneous texture; it is a brecciated enstatite Moderate weathering grade. Specimens: 7.8 g, NAU; main orthopyroxenite with a series of prominent, parallel mass, Oakes. compression fractures (0.1 to 0.8 mm spacing) that span the entire sample. These fractures acted as conduits for Northwest Africa 1665 weathering; most weathering effects are limited to areas that Northwest Africa border these fractures. Mineral modes: enstatite, 92 vol%; Si- Found 2002 bearing metal, 4%; plagioclase (maskelynite), 2%; high-Cr Carbonaceous chondrite (CK3 anomalous) troilite, 2%; graphite, <1%. Enstatite, FeO = 0.03 to A single stone of 1185 g covered by fusion crust was found in 0.64 wt%; CaO = 0.06 to 0.38 wt%.; Cr-rich troilite, Cr = 10.2 2002 by an anonymous finder in the western Saharan desert. to 14.7 wt% with Mn <1.15% and Ti <1.76 wt%. The largest Classification and mineralogy (A. Greshake and M. Kurz, metal grains (0.6–1.0 mm in diameter) have graphite MNB): it is a type 3 carbonaceous chondrite with chondrules, inclusions <0.1 mm in size; metal, Ni = 6.5 wt% (range = 6.2– irregular shaped olivine-rich objects, and mineral fragments 6.9), Si = 1.25 wt% (range = 0.9–1.81); plagioclase, An42. set into a fine-grained matrix of Fe-rich olivine, Ca pyroxene, None of the exotic sulfides common to and enstatite troilite, and Fe-Ni metal; chondrules have a mean diameter of chondrites were found. Shock level, S4 (parallel fractures, 130 µm and porphyritic olivine and pyroxene chondrules reduced birefringence, and mottled extinction in enstatite; all clearly dominate over radiating or cryptocrystalline types; plagioclase is maskelynite); weathering grade is W2/3. matrix abundance is about 50 vol%; olivine, Fa25.7 (the range Specimens: type specimen, 21.1 g, NAU; main mass, Oakes. is Fa0.7–37.6); pyroxene, Fs12 (the range is Fs2.5–48.3); oxygen isotopic compositions (R. Clayton and T. Mayeda, UChi): Northwest Africa 2042 δ18O = –1.03‰, δ17O = –4.95‰ and (I. Franchi and R. C. Morocco Greenwood, OU): δ18O = –1.88‰, δ17O = –5.43‰, ∆17O = – Purchased 2003 October 4.45‰ are clear of the CO3 chondrite field and possibly located on an extension of the CK3 range; shock stage, S1; An uncrusted stony- (700 g) with a brown, weathering grade, W2. Specimens: Main mass with weathered surface was purchased in Erfoud by a Moroccan anonymous finder; type specimen 22 g plus one polished thin dealer for D. Gregory (Gregory) in 2003 October. section, MNB. Classification and mineralogy (A. Irving and S. Kuehner, UWS): subequal amounts of metal and silicates in a coarse- Northwest Africa 1839 grained plutonic igneous texture. The metal has rounded Morocco grains of taenite (30 wt% Ni) within dominant kamacite Found 2003 (5 wt% Ni). The remainder of the sample consists mainly of Ordinary chondrite (L7) orthopyroxene (Fs26.1Wo2.1 to Fs25.7Wo3.9; FeO/MnO = 17.8– A 121.8 g, partially crusted stone was purchased in Rissani, 20.3) and anorthitic plagioclase (An95.8) with accessory Morocco in June 2003. Description and classification (T. chromite, troilite, and a silica polymorph. This sample Bunch and J. Wittke, NAU): the meteorite contains polygonal, appears to be paired with NWA 1817 and NWA 1878 (see A212 S. S. Russell et al.

Bunch et al. 2004). Specimens: type specimen, 20 g, UWS; Chondrules are less than 2 mm in diameter and are poorly main mass, Gregory. abundant (<20%). CAIs (anorthite, spinel, and melilite) are different sizes and up to 1 cm. The fine-grained matrix is very Northwest Africa 2085 abundant. Chondrules consist of non-equilibrated porphyric Morocco olivine (Fa0.7–28), or opx (Fs0.91), glass, magnetite, pentlandite Found 2003 October and a few rare spherules of iron metal in the olivine crystals. Ordinary chondrite (L melt rock) Anorthite occurs in the center part of some opx chondrules A 2.7 kg single stone was purchased in Rissani, Morocco. (An85Ab16), associated with fassaite (Fs08Wo44) and Description and classification (T. Bunch and J. Wittke, NAU): hedenbergite (Fs42Wo50). In the matrix the olivine is Fa55–91. exceptional melt rock: cm-size clasts are Specimens: type specimen, 23.6 g, MNHNP; plus 4 g and thin surrounded by crystallized melt. The melt contains oblate to sections, UJM, main mass with finders. round, eutectic-textured, masses (up to 2.5 mm) of taenite metal set in troilite. The metal/troilite complexes show strong Northwest Africa 2286 flow alignment in a matrix of tabular to equant olivine Northwest Africa (<0.8 mm), which has no apparent preferred orientation, and Purchased 2003 SiO2-rich glass, in addition to small, recrystallized chondrite Achondrite (olivine-rich ) fragments. Melt olivine, Fa22.8 (range Fa22.1–23.8); taenite, Ni = A single stone of 82 g was found 2003 by an anonymous 15.4 wt%, range, 13.6–16.1 wt%; troilite, Ni = 0.42 wt%; finder in the western Sahara and purchased in 2003 in glass, SiO2 = 74.6 wt%, FeO = 3.6 wt%. Clast chondrules and Morocco. Classification and mineralogy (A. Greshake, matrix are partially recrystallized from shock effects; olivine, MNB): dominated by large blocky orthopyroxene crystals and Fa22.2–23.9; orthopyroxene, Fs18–19.9Wo1.4–2.0. Shock level, S4 ~20% large olivine phenocrysts; minor phases include FeS, to S6; weathering grade, W1/2. Specimens: type specimen and Fe-Al-Cr-spinel; orthopyroxene, Fs21.9Wo1.5, olivine, 88.5 g, and one thin section, NAU; main mass, Farmer. Fa26.8; low degree of shock; moderately to strongly weathered and very friable; most likely paired with NWA 1877. Northwest Africa 2251 27°58′N, 7°57′W Specimens: main mass with anonymous finder; type Found 2001 October specimen 23.5 g plus one polished thin section, MNB. Achondrite () A fusion-crusted stone of 17 g was found by nomads on Northwest Africa 2289 October 2001 near Tindouf (western Algeria). Mineralogy Northwest Africa and classification (A. Seddiki, UO/UJM; B. Moine, J. Y. Purchased 2003 Cottin, UJM; V. Sautter, J. P. Lorand, M. Denise, MNHNP): Rumuruti chondrite (R3–6) Cumulate eucritic and diogenitic clasts in a clastic matrix. A single stone of 46.5 g was found in 2003 by an anonymous clasts contain plagioclase An90 (range An88–92), finder in Western Sahara. Classification and mineralogy (A. pigeonite (Fs43–53Wo6–20) with exsolved augite (Fs37Wo25). Greshake, MNB): a brecciated type 3–6 Rumuruti chondrite; Minor minerals are a silica phase, troilite, Ti chromite (TiO2 = olivine, Fa13.5–40.5; low-Ca pyroxene, Fs3.7–29.1Wo0.2–4.3; 1.65 wt%) and ilmenite. Diogenite clasts are composed by augite, Fs10.5Wo47.2; plagioclase, An8.8–22; low degree of orthopyroxene (Fs32–36Wo2–4) with augite exsolution lamellae shock; low to moderately weathered. Specimens: main mass (Fs42Wo46), chromite, troilite, and ilmenite. The Fe/Mn with anonymous finder; type specimen 10.2 g plus one atomic ratio in pyroxenes ranges from 24 to 30. Eucritic clasts polished thin section, MNB. comprise <60 vol% of the rock. The analyses of the glass in the fusion crust corresponds to the bulk compositions of Northwest Africa 2353 . The oxygen isotopic composition (δ18O = Northwest Africa +5.2‰, δ17O = +2.3‰, ∆17O = –0.4‰) confirms that this Purchased 2004 rock belongs to the HED suite, although the ∆17O is slightly Achondrite (ungrouped) lower than the HED grand mean. Specimens: main mass 16 g, A stone of 580 g was purchased in Erfoud, Morocco. MNHNP, thin section, UJM. Description and classification (T. Bunch and J. Wittke, NAU): completely recrystallized into polygonal and subhedral Northwest Africa 2269 27°55′N, 7°50′W grains; H-group chondrite affinities, but with different oxygen Found 2002 March isotopes, no relict chondrules; grain size <0.5 mm, mean = Carbonaceous chondrite (CV3) 0.2 mm; intensely fractured with abundance of subparallel The meteorite, found by nomads near Tindouf (southwest compression fractures. Olivine and pyroxene analyses are Algeria), weighs 184 g, and is completely covered by a fusion within the precision of the electron microprobe. Olivine, crust. Mineralogy and the classification (A. Seddiki, UO/ Fa17.9, FeO/MnO = 34; NiO = 0.35 ± 0.12 wt%; UJM, B. Moine, J. Y. Cottin, UJM; M. Denise, MNHNP). orthopyroxene, Fs15.6Wo3.1, FeO/MnO = 19; plagioclase, The Meteoritical Bulletin No. 89 A213

An13.1Or2.6; chromite, cr# = 87; FeS, Ni = 1.65 wt%; metal Northwest Africa 2379 (taenite only), Ni = 21.6 wt%; trace amount of merrillite; Northwest Africa magnetite: NiO = 0.27 ± 0.10 wt%. Oxygen isotope replicate Purchased 2004 August analyses (T. Larson and F. Longstaffe, UWO) of acid-washed, Achondrite (howardite) bulk sample by laser fluorination gave δ17O = +3.16‰, A 68 g stone with fusion crust was purchased in Erfoud, +3.3‰, δ18O = +5.10‰, +5.51‰, and ∆17O = +0.44‰, Morocco. Description and classification (T. Bunch and J. +0.51‰. Weathering grade, W3 and lightly shocked (S2). Wittke, NAU): an unusual howardite that contains an array of Specimens: type specimen, 20.1 g NAU; main mass, plastically deformed shocked eucrite and diogenite clasts. Regelman. Shock characteristics range from crushed cataclastics (S2–4), maskelynite-bearing (S4), recrystallized pyroxenes and Northwest Africa 2372 plagioclase (S5) to melt clasts (S6) that contain olivine as the Northwest Africa quenched mafic phase in place of typical pyroxenes. Found 2004 : orthopyroxene, Fs25.0Wo2.9 (FeO/MnO = 29.4); Carbonaceous chondrite (CK4) plagioclase, An88.8; chromite, cr# = 76, mg# = 24. : A 440 g single, brownish stone was purchased in Erfoud, orthopyroxene, Fs47.8–61.4Wo1.4–2.3 (FeO/MnO = 31.2–36); Morocco in May 2004. Description and classification (T. pigeonite, Fs51.3–56.8Wo7.7–12.6; augite, Fs27Wo28.1; Bunch and J. Wittke, NAU): contains ~33 vol% chondrules plagioclase, An86.4–91.1. Quench olivine (<0.05 mm in that are typically smaller than most CK meteorites (<1 mm in diameter): cores, Fa17.9; rims, Fa36.4 (FeO/MnO = 41–47); low diameter), abundant melilite-spinel CAIs rimmed by weathering grade. Specimens: type specimen, 13 g, NAU; subcalcic augite, and partially recrystallized matrix. Matrix main mass, G. Hupé. olivine, Fa29.5–34.2, FeO/MnO = 30.8–37.8 NiO = 0.35 ± 0.12%; low-Ca pyroxene, Fs25.3–29.0Wo0.9–5.3, FeO/MnO = Northwest Africa 2381 25.3–29.0; plagioclase, An36.8–51.2Or1.7–3.0; magnetite, Cr2O3, Northwest Africa = 5.3 wt%, Al2O3, 5.3 wt%, TiO2 = 1.97 wt%, NiO= 0.27 ± Purchased 2004 August 0.1%, troilite, and Fe-, Mg-rich feldspathic glass. A portion of Ordinary chondrite (LL melt breccia) the glass has been replaced by terrestrial carbonate. Shock A 132 g complete and crusted stone was purchased in Erfoud, level is S2, weathering grade, W3. Specimens: type specimen, Morocco. Description and classification (T. Bunch and J. 23 g NAU; main mass, Reed. Wittke, NAU): highly shocked (melted and brecciated) LL chondrite (S2–6). Contains sparse marble-shaped (0.8– Northwest Africa 2373 1.4 mm) LL7 clasts that show equigranular, recrystallized Northwest Africa texture with abundant 120° triple grain junctions. Olivine, Purchased 2004 August Fa31.8 (FeO/MnO = 63); orthopyroxene, Fs25.1Wo1.8; Martian meteorite (olivine-phyric shergottite) chromite, cr# = 86, Fe# = 92. Clasts are enclosed by a thick Several small stones that weigh 18.1 g were purchased in mantle (up to 5 mm) of LL chondrite, similar in composition, Erfoud Morocco. They are yellow brown with desert ablation/ but without recrystallization (shock level = S3). These varnish surface only, no fusion crust. Description and mantles are surrounded by highly shocked LL materials that classification (T. Bunch and J. Wittke, NAU): olivine range from complete melt with quench products of olivine, Ca phenocrysts (<1.25 mm in longest dimension) set in a fine- pyroxenes, and feldspathic glasses (S6) to intense, shock grained groundmass (<0.1 mm) of pigeonite, maskelynite, darkened LL clasts (metal melt with injection and chromite, Ti magnetite, augite, chlorapatite and sulfide. maskelynite, S4). Weathering grade is W2. Specimens: type Olivine has cores of Fa30.7 (FeO/MnO = 51.9), rims of Fa50.3 specimen 21 g NAU; main mass, G. Hupé. (FeO/MnO = 53.3) and contain micron to submicron inclusions of chromite, glass, and barite. One large olivine Northwest Africa 2386 grain, which may be a xenocryst, is different from the rest Northwest Africa with a core of Fa29.1 (FeO/MnO = 43) and more abundant tiny Purchased 2004 September inclusions. The wide (0.2 to 0.4 mm), inclusion-free mantle Carbonaceous chondrite (CK4) on this grain is Fa32.3 (FeO/MnO = 39.2). Pigeonite is zoned A 440 g single stone with weathered crust was purchased in from Fs29.4Wo8.4 to Fs36.4Wo14.1 (FeO/MnO = 28); augite is Erfoud, Morocco. Description and classification (J. Wittke Fs21.8Wo29.1. Maskelynite is slightly zoned with a and T. Bunch, NAU): contains ~42 vol% small chondrules compositional average of An52.1Or2.1. Chromite, cr# = 87, fe# with ~13 vol% CAI components dominated by melilite-spinel = 90.4. Overall texture, mineral content and mineral aggregates, rimmed by diopside or subcalcic augite. compositions strongly suggest that this stone is paired with Chondrules have well-defined rims and mostly crystallized NWA 1068. The specimen is lightly weathered and mesostasis. Matrix is partially recrystallized with minor Fe-, moderately shocked. Specimens: type specimen, 3.7 g and Mg-rich feldspathic glasses. Olivine is fine-grained and one thin section, NAU; main mass, Birdsell. poorly crystallized. Matrix olivine, Fa29.5–34.8 (FeO/MnO = A214 S. S. Russell et al.

31–37); low-Ca pyroxene, Fs25.3–29.0Wo0.9–5.3 (FeO/MnO = mineral compositions, and oxygen isotope composition NWA 25.3–29.0); plagioclase, An41.0–51.2Or2.1–2.9; magnetite, Cr2O3 2400 is nearly identical to the anomalous achondrite NWA = 5.3 wt%, Al2O3 = 1.86 wt%, TiO2 = 1.97 wt% and NiO = 011 (Yamaguchi et al. 2002; Promprated et al. 2003), which 0.31 wt%. Moderately weathered and lightly shocked (S2). strongly indicates that these two stones are paired. Specimens: type specimen, 22 g NAU; main mass, Reed. Specimens: type specimen 20.2 g and three polished thin sections, NAU; main mass, anonymous purchaser. Northwest Africa 2388 Northwest Africa Northwest Africa 2428 Purchased 2004 September Northwest Africa Carbonaceous chondrite (CK6) Found 2004 An 81 g fresh and fully crusted stone was purchased in Iron (IAB) Erfoud, Morocco. Description and classification (T. Bunch A single mass with a total weight of 1650 g was purchased in and J. Wittke, NAU): fully equilibrated and recrystallized Erfoud, Morocco in July, 2004. Description and classification with a few indistinct, relict chondrules. Abundant plagioclase (John Wasson, UCLA): NWA 2428 is a plessitic forms a discontinuous network around enclaves of olivine, Ca that has suffered some post-shock recrystallization. It is pyroxene, and magnetite matrix and around relict chondrules. dominated by long (~2 cm) schreibersite lamellae that are Olivine in matrix and chondrules is very homogeneous, surrounded by swathing kamacite ~0.6 mm thick (Fig. 1). Fa31.9–32.6 (N = 26) and very low MnO contents (FeO/MnO = Shock has caused fractures near most of the schreibersite 113–137); Ca pyroxene, Fs20.5Wo50.5 (FeO/MnO = 98–118); lamellae. Weathering is minor. Cr 22 µg/g, Co 5.58 mg/g, Ni plagioclase, An85.9Or7.4. All silicates contain NiO: olivine, 117.7 mg/g, Cu 200 µg/g, Ga 16.8 µg/g, As 28.3 µg/g, Sb 0.62–0.82 wt%, Ca pyroxene, 0.78–1.09 wt%, plagioclase, 180 ng/g, W 0.17 µg/g, Ir 1.09 µg/g, Au 2.646 µg/g. Based on 0.41–0.49 wt%. Magnetite, Cr2O3 = 5.3 wt%, Al2O3 = these data, the meteorite can be classified as a IAB, subclass 2.36 wt%, NiO = 0.51 wt%. Moderately weathered and low HL, iron (Wasson et al. 2002). Specimens: type specimen, shock level. Specimens: type specimen, 16.2 g NAU; main 55 g UCLA, main mass, Birdsell. mass, Reed. Northwest Africa 2434 Northwest Africa 2400 Northwest Africa Morocco or Algeria Purchased 2004 Purchased 2003 April Achondrite (diogenite, metal-rich) Achondrite (ungrouped) A 441 g partially crusted stone was purchased in Erfoud, A 137 g light tan to rusty-brown, fully crusted stone was Morocco. Description and classification (J. Wittke and T. purchased in Rissani, Morocco in April 2003. Description and Bunch, NAU): highly brecciated, metal-rich diogenite with classification (T. Bunch and J. Wittke, NAU; A. Irving and S. orthopyroxene fragments up to 11 mm in size and scattered Kuehner, UWS): composed mainly of approximately mm- recrystallized pockets. Modal content in vol%: sized, randomly oriented pigeonite (Fs64–64.8Wo5.6–6.4) with orthopyroxene, 86.2; metal, 7.3 (heterogeneously distributed, very fine, parallel exsolution lamellae of augite (Fs38–49.1 4.3 to 13.2 vol%); plagioclase, 5.5, phosphate, sulfide and Wo36.7–23), and interstitial, recrystallized plagioclase (<0.10 chromite <2. Orthopyroxene, Fs24.2Wo1.3 (FeO/MnO = 32.7); mm in size, ~An86Or0.5) with prominent triple junctions, and Ca-rich pyroxene, Fs8Wo46.9; plagioclase, An95.7; chromite, rare, unrecrystallized, tabular plagioclase relicts (<1 mm, cr# = 69; metal, Ni = 6.5 wt%. Very fresh; shock level, S2. zoned from An80 to An89). FeO/MnO ratios for all pyroxenes Specimens: type specimen, 27.6 g NAU; main mass, Hall. range from 59.5 to 68.7 (avg. 64.7). Only small amounts of pyroxene are present in the recrystallized zones. Accessory Northwest Africa 2480 minerals occurring predominantly in the recrystallized Northwest Africa plagioclase zones include a silica polymorph, chromite [Cr/ Found 2004 (Cr + Al) = 83, Fe/(Fe + Mg) = 67], ilmenite (53.5 wt% TiO2, Achondrite (howardite) 43.6 wt% FeO; with small baddeleyite inclusions), merrillite A single stone of 4.1 g almost completely covered with fusion (some with minor amounts of Na2O, MgO, and FeO), Zn- crust was found spring 2004 by an anonymous finder in the bearing troilite, pentlandite, Cr ulvöspinel and altered Fe Sahara and purchased March 2004 in Rissani. Classification metal (associated with minor troilite, barite, and calcite). and mineralogy (A. Greshake, MNB): polymict breccia with Shock damage is not apparent and, with the exception of the basaltic eucrite and diogenitic clasts are set into a more fine- oxidation of minor metal, weathering effects are very low. grained clastic matrix; dark impact melt fragments are rare; Oxygen isotopes (D. Rumble, CIW): replicate analyses by eucrite clasts contain plagioclase, An92.9 (range An87.9–96.8) 17 18 laser fluorination gave δ O = –0.15 0.1‰, δ O = +3.27 and pigeonite, Fs25.8Wo8.7; minor phases include Al-Ti 0.2‰, ∆17O = –1.57 ± 0.03‰. In its texture, mineral mode, chromite and troilite; diogenite clasts are composed mainly of The Meteoritical Bulletin No. 89 A215

orthopyroxene, Fs26.9–31.9Wo2.4–3.9; high degree of shock; low direction with some small masses poikilitically enclosed by degree of weathering. Specimens: type specimen 1.15 g plus large pigeonite. The degree of olivine-pigeonite reduction is one polished thin sections MNB. low to moderate. Olivine cores, Fa20.3 (Cr2O3 = 0.72 wt%), rims are Fa8–10.8 (Cr2O3 = 0.53 wt%); pigeonite, Fs17.4Wo7.6 Northwest Africa 2519 (Cr2O3 up to 1.56 wt%). Weathering is low grade and the Algerian-Moroccan border shock level is S2. Specimens: type specimen, 22.2 g NAU; Found 2004 main mass, G. Hupé. Carbonaceous chondrite (CK4) One completely crusted stone weighing 44.5 g was purchased Northwest Africa 2626 in Erfoud in September 2004. Classification and mineralogy Northwest Africa (M. Bourot-Denise, MNHNP): clear chondritic texture, with Purchased 2004 November large chondrules (~500 µm) and large opaque nodules of Martian meteorite (basaltic shergottite) associated pentlandite and magnetite with minor pyrrhotite. A 31.07 g completely crusted stone was purchased by Silicates are generally very fissured and blackened by fine Farmer. Classification and mineralogy (J. Wittke and T. magnetite blebs. Their composition is very homogeneous; Bunch, NAU; A. Irving and S. Kuehner, UWS): olivine- olivine Fa31.3 ± 0.4, 0.5 wt% NiO; pyroxene Fs27.0 ± 1.1Wo1.6 ± 2.0; orthopyroxene-phyric basaltic rock composed of euhedral to clinopyroxene Fs9.1Wo46.9; plagioclase An22 to An47, 0.13 wt% subhedral olivine phenocrysts and preferentially-oriented, NiO. Magnetite is Cr-rich, 4.3 wt% Cr2O3, 0.6 wt% NiO, 0.3 prismatic low-Ca pyroxene phenocrysts in a groundmass of wt% TiO. Estimated shock stage S3, weathering grade W2 zoned pigeonite (Fs26.4Wo12.4 to Fs34.1Wo12.4) FeO/MnO = (sulfide altered); magnetic susceptibility 4.61 (J. Gattacceca, 27–31; maskelynite (An66.0–71.0Or0.4), olivine (Fa43.6–47.3) CEREGE). Specimens: type specimen 9.4 g and one polished FeO/MnO = 51–58; Ti chromite (Cr/(Cr+Al) = 0.72–0.79; mount, MNHNP; main mass, Thomas. 9.2–19.8 wt% TiO2), chromite (Cr/(Cr+Al) = 0.71–0.86; 0.7– 2.0 wt% TiO2), merrillite, ilmenite, ulvöspinel and pyrrhotite. Northwest Africa 2520 Olivine phenocrysts are zoned from Fa16.7 cores to Fa43.3 Algeria rims, and pyroxene phenocrysts have irregular cores of Found 2004 orthopyroxene (as magnesian as Fs17.9Wo2.4, with ~0.03 wt% Ordinary chondrite (LL3) TiO2 and ~0.4 wt% Al2O3) mantled by pigeonite (Fs25.4Wo4.4 One partially crusted stone, weighing 75.5 g, was purchased to Fs37.0Wo12.7) with minor subcalcic augite (Fs21.7–24.0 in Erfoud in September 2004. Classification and mineralogy Wo30.8–31.1). It is apparently not terrestrially paired to NWA (M. Bourot-Denise, MNHNP): brecciated; major part has 1195 and NWA 2046 (Irving et al. 2004b; 2005). Specimens: abundant, large chondrules (>500 µm), with entirely type specimen, 6.4 g, and one polished thin section, NAU; devitrified mesostasis (diopside and plagioclase, An12.3); one polished thin section, UWS; main mass, anonymous. several more or less melted clasts, in which the chondritic texture has been erased and opaques make up pervasive fine Northwest Africa 2627 blebs in silicates. Olivine, Fa0.9–32.3, mean Fa25.0 ± 7.7, FeO- Northwest Africa poor chondrule olivines are zoned; pyroxene, Fs3.5–33.7, mean Found 2004 Fs18.2 ± 8.9. Magnetic susceptibility 3.66 (J. Gattacceca, Achondrite (acapulcoite) CEREGE). Estimated subtype 3.6–3.7 (from FeO zoning in A 68 g mostly crusted, partial stone was purchased in Erfoud olivine); estimated shock stage S4/S5; weathering grade W4 in October 2004. Description and classification (T. Bunch (metal and sulfide much altered). Specimens: type specimen and J. Wittke, NAU): recrystallized into polygonal and 15.8 g and one polished mount, MNHNP; main mass, subhedral grains with the exception of large orthopyroxene Thomas. grains (up to 3 mm) that poikilitically enclose olivine; heavily fractured, variable grain size, and heterogeneous Northwest Africa 2625 distribution of phases. Modal analyses (vol%): Northwest Africa orthopyroxene, 44; olivine, 41; FeS, 6; metal (and Fe oxides), Purchased 2004 August 5; plagioclase, 3 and minor merrillite, Ca pyroxene and Achondrite (ureilite) chromite. All silicates have very homogeneous compositions; A 305 g single stone was purchased in Erfoud, Morocco. olivine, Fa13.1 (FeO/MnO = 26); orthopyroxene, Fs12.2Wo2.7 Description and classification (J. Wittke and T. Bunch, NAU): (FeO/MnO = 13.9); plagioclase, An21.9; metal, Ni = 6.7 wt% medium- to coarse-grained (<4 mm), typical ureilite with Ni. Oxygen isotopes (D. Rumble, CIW): replicate analyses of pronounced preferred orientation of silicates, which are acid-washed whole rock material by laser fluorination gave mostly elongated with curvilinear morphology. Pigeonite δ17O = 1.82, 1.75, 1.47, 1.56‰; δ18O = 4.93, 4.96, 4.51, shows well-defined twinning; graphite and carbonaceous- 4.51‰; ∆17O = –0.781, –0.865, –0.908, –0.821‰. metal-silicate masses tend to cross trend the lineation Weathering grade is W2/3 with ferric Fe staining; shock level A216 S. S. Russell et al. is low to moderate. Specimens: type specimen, 13.7 g NAU: texture, 24, subophitic basalts, 6 other, 5. Diogenite main mass, Strope/Farmer. orthopyroxenes, Fs12.7–24Wo0.6–2.7 (FeO/MnO = 27.1–30.3); cumulate basalts, Fs29–57.4Wo1.9–3.7; cumulate basalt chromite, Northwest Africa 2635 cr# = 82. Shock level moderate, low weathering grade. Northwest Africa Specimens: type specimen, 18.8 g NAU; main mass, Reed. Purchased October 2004 Achondrite (ungrouped) Northwest Africa 2644 A 4.2 kg, partially crusted stone was purchased in Erfoud, Northwest Africa Morocco. Description and classification (T. Bunch and J. Purchased 2004 Wittke, NAU), results from one thin section (2.4 cm2): mostly Achondrite (howardite) recrystallized into fine-grained (<0.5 mm, avg. = 0.185 mm) A 216 g dark, crusted stone was purchased in Erfoud, polygonal and subhedral grains with the exception of several Morocco in August 2004. Description and classification (T. medium to large (1.2–3.0 mm) orthopyroxene grains that Bunch and J. Wittke, NAU): composed of typical cumulate contain very small olivine (<0.1 mm) inclusions. Olivine and and basaltic eucrite clasts and large (up to 2.8 mm in orthopyroxene analyses are homogeneous within the diameter), very dark shock-melt and breccia clasts of glass, precision of the electron microprobe (±0.15 mol%) and quench crystals, and shocked diogenite and eucrite fragments, indicate affinities. Olivine, Fa18.9 (FeO/MnO = all set in a very light-colored and fine-grained matrix. In 38.1); orthopyroxene, Fs16.8Wo2.9 (FeO/MnO = 20.0); addition, irregular to sub-rounded metal grains up to 3 mm in plagioclase, An15.1Or4.7; metal (only taenite found), Ni = diameter are present within the shocked clasts and randomly 18.9 wt%; chromite (only one grain found), cr# = 84.5; FeS, distributed in the matrix. Diogenite orthopyroxene, Fs21.3–29 Ni = 1.42 wt% and Co = 0.28 wt%, minor merrillite. Most Wo0.8–3.1 (FeO/MnO = 24.5–32.4); shocked clast pigeonite, metal has been oxidized; specimen contains ~70% olivine Fs29.1–31.8Wo3.4–6.1 (FeO/MnO = 30.2=33.4); cumulate implying it contained less metallic iron than an H chondrite pyroxene, Fs51.4–56.4Wo2.9–3.8; large plagioclase fragments, when fresh. Oxygen isotope replicate analyses (D. Rumble, An90–94.2; metal, Ni = 4.4–18.3 wt%. Low-grade weathering CIW) of acid washed, bulk sample by laser fluorination gave and low level shock; shock-melt/breccia clasts experienced δ17O = +3.23‰, +2.98‰, δ18O = +5.03‰, +4.37‰ and ∆17O high shock levels. Specimens: type specimen, 22.0 g NAU; = +0.614‰, +0.708‰. Weathering grade, W4 with staining; main mass, Oakes. shock level, low. Specimens: type sample, 23.2 g NAU; main mass, Strope/Farmer. Northwest Africa 2645 Northwest Africa Northwest Africa 2639 Purchased 2004 Northwest Africa Enstatite chondrite (EL6) Purchased 2004 A single stone of 166 g was purchased in Erfoud, Morocco. Mesosiderite Description and classification (J. Wittke and T. Bunch, NAU): Three complete stones weighing 539 g in total with black to cataclastic, fine-grained (<0.20 mm) with very rare relict brown surfaces, were purchased in Erfoud, Morocco. chondrule fragments. Contains orthopyroxene, Fs1.6Wo1.4; Description and classification (T. Bunch and J. Wittke, NAU): plagioclase, An5.4–11.1Or0.7–5.4; metal. Ni = 3.75 wt%, Si = mesosiderite with nearly equal portions of metal and silicates; 0.93–1.45 wt%, troilite, Ti = 3.1 wt%, schreibersite, and metal composed of mostly continuous aggregates of metal daubreelite. Shock level is S2 and the weathering grade is W3 balls (0.2–0.4 mm in diameter) that resemble grape clusters with moderate staining. Specimens: type sample, 21.3 g NAU; and enclose clumps of silicates. Orthopyroxene, Fs23.1–25.5 main mass, Oakes. Wo1.7–3.3 (FeO/MnO = 23.5–27.9); plagioclase, An88.9; chromite, cr# = 82; metal, Ni = 6.1–7.0 wt%, merrillite and Northwest Africa 2677 troilite. Shock level moderate and a weathering grade of W1. Northwest Africa Specimens: type specimen, 21.1g NAU; main mass, A. Hupé. Found 2004 Iron (IIICD) Northwest Africa 2641 A single mass with a total weight of 100 g was purchased in Northwest Africa Erfoud, Morocco in September 2004. Description and Purchased 2004 classification (Andrew Campbell, UChi): the meteorite is a Achondrite (howardite) fine octahedrite, Fe, wt% 86.5, Co, wt% 0.585, Ni, wt% 12.8, A complete and crusted 9 g stone was purchased in Erfoud, Ga 7.8 ppm, Mo 3.81 ppm, Ru 0.174 ppm, Rh 0.211 ppm, Pd Morocco. Description and classification (T. Bunch and J. 6.6 ppm, W 0.135 ppm, Re 0.010 ppm, Os 0.058 ppm, Ir Wittke, NAU): Fine to medium-grained (≤1.5 mm) howardite 0.066 ppm, Pt 0.131 ppm, Au 1.83 ppm. Specimens: type with a modal content of (in vol%): diogenites, 65; cumulate specimen, 17 g UCLA, 4 g UChi; main mass, Birdsell. The Meteoritical Bulletin No. 89 A217

Northwest Africa 2738 847 µm); coarse grained rims of chondrule minerals; metal- Algeria rich porphyritic olivine; amoeboid olivine aggregates. Olivine Found 2002–2003 (n = 45; mean Fa9.56; range Fa0.02–24.36; two peaks at Fa0–2 and Achondrite (howardite) Fa9–13). Orthopyroxene: (n = 5, Fs4.62–9.33Wo0.15–1.21); low-Ca One single stone of 370 g mostly covered with fresh fusion clinopyroxene: (n = 6, Fs16.98–35.86Wo1.04–5.66, Cr2O3: 0.24– crust was found in the winter of 2002/2003 by an anonymous 1.04 wt,%, MnO 0.27–0.76 wt%). Weathering grade: W3, finder in the western Sahara. Classification and mineralogy shock stage: S2. Specimens: type specimen 21.5 g, Ham, (V. Moggi-Cecchi and G. Pratesi, MSP): polymict breccia with main mass, Burkard. cumulate eucrite and diogenite fragments, not exceeding 10% of the total surface. Orthopyroxene fragments are commonly Northwest Africa 2815 found set into a clastic matrix. Other types of fragments Morocco(?) include large blocky plagioclase, An89.58Ab9.95Or0.47, augite Found 2003 exsolution lamellae, Fs27.52En28.84Wo43.64, and low-Ca Mesosiderite pyroxene clasts (Fs59.84En35.27Wo4.89); minor phases are A single stone of 147 g was found by Moroccan nomads and sulfides and Fe-Ni metal. Oxygen isotope data (I. Franchi, R. sold in Morocco. Mineralogy and classification (J. Schlüter, Greenwood, OU): δ17O = +1.754‰; δ18O = +3.731‰; ∆17O = Ham): orthopyroxene clasts up to several mm in size in a fine –0.186‰ point to interpretation as HED even if the ∆17O value grained matrix of feldspar and pyroxene. Subequal amounts of is slightly more positive than the mass fractionation line for metal and silicates. Anorthite (n = 5, An91.81–96.30Ab3.58–8.19 HEDs, probably due to terrestrial contamination. The degree Or0–0.26); orthopyroxene (n = 7, Fs18.21–35.10Wo0.99–3.94, FeO/ of shock is low as well as weathering. Specimens: main mass MnO = 29.16–37.05); low-Ca clinopyroxene (n = 3, Fs35.92– with anonymous finder; type specimen 30 g plus one polished 44.76Wo1.81–5.06); one olivine grain with mg#: 84.8; one high-Ca thin section, MSP. clinopyroxene Fs22.7En39.2Wo38.1. Orthopyroxene to plagioclase ratio and chemistry indicate class A; texture type 2. Northwest Africa 2739 Weathering grade: W2, shock stage: S2. Specimens: type Algeria specimen 23.2 g, Ham, main mass, Burkard. Found 2002–2003 Achondrite (howardite) Northwest Africa 2821 Four stones weighing 824 g in total covered with fresh fusion Morocco crust were found in winter 2002/2003 by an anonymous Found 2003 finder in the western Sahara. Classification and mineralogy Rumuruti chondrite (R3.8) (V. Moggi-Cecchi and G. Pratesi, MSP): polymict breccia A single stone of 384 g was purchased from Moroccan mainly with cumulate eucrite fragments; diogenite fragments mineral and fossil dealers in 2003. It was probably found in not exceed 10% of the total surface. Orthopyroxene crystals, the Zagora region of Morocco. Mineralogy and classification commonly set into a clastic matrix, are the main silicate (J. Schlüter, Ham): the sample is brecciated; olivine phase. Their compositions vary from more Fe-rich terms fragments in matrix Fa39.25 ± 0.63 (range Fa38.5–40.6, n = 11), (Fs24.43En73.90Wo1.67) to more Mg-rich terms olivine in chondrules Fa37.52 ± 5.85 (range Fa17.3–40.7, n = 22), (Fs12.18En87.66Wo0.16). Other types of fragments include large NiO in olivine, average 0.16 wt%; orthopyroxene Fs13.79 ± 8.52 plagioclase (An92.52Ab7.00Or0.48) and augite; minor phases are (range Fs6.55–30.1, n = 6); clinopyroxene (mean sulfides and Fe-Ni metal; a chromite grain with Cr/(Cr+Al) = Fs10.95En45.36Wo43.68, n=3). Chromium spinel (mean, n = 2: 0.88 and Fe:Mn:Mg ratios = 0.85:0.02:0.13) is also present. FeO 40.51, MgO 0.97, MnO 0.34, Al2O3 5.05, Cr2O3 44.15, Oxygen isotope measurements (I. Franchi, R. Greenwood, TiO2 5.81). Chondrule size (n = 35, 405 µm). Weathering OU): δ17O = +1.554‰; δ18O = +3.439‰; ∆17O = –0.234‰ grade: W3, shock stage: S2. Specimens: type specimen, 21.8 plot in the HED area, with a slightly more negative value. g, Ham, main mass Herkstroeter. Shock degree is low as well as degree of weathering. Specimens: main mass with anonymous finder; type Northwest Africa 2873 specimen 35 g plus one polished thin section, MSP. Morocco Found 2002 Northwest Africa 2812 Achondrite (howardite) Region El Mahabas, S of Zag, Morocco One fresh-looking stone, weighing 36 g, covered with a Found 2003 cracked fusion crust, was purchased in Morocco. Carbonaceous chondrite (CR) Classification and mineralogy (M. Bourot-Denise, MNHNP): A single stone of 355 g was found by Moroccan nomads and breccia composed of a relatively fine-grained matrix made up sold in Morocco. Mineralogy and classification (J. Schlüter, of angular crystals, in which 3 kinds of mm-sized clasts are Ham): abundant well defined chondrules (n = 40: mean embedded: diogenitic clasts (pyroxene, plagioclase), basaltic A218 S. S. Russell et al. eucritic clasts (pigeonite, augite, plagioclase), and granular- Rissani, Morocco in 2002. Description and classification (J. textured eucritic clasts. Minor phases include silica in small Wittke and T. Bunch, NAU): mostly even-sized (1–2 mm) areas, associated with opaques (ilmenite, chromite, chondrules are slightly flattened and define a preferred pyrrhotite, rarely metal). Dominant diogenitic orthopyroxene, orientation. A few chondrules are completely rimmed by Fs22.3Wo1.8; associated plagioclase An83–95. Eucritic metal (Ni = 6.3 wt%). The matrix contains numerous round pyroxene, Fs35.1Wo5.8–Fs52.3Wo18.3. Low shock stage; metal grains (0.3 to 1.8 mm diameter) and smaller (<0.4 mm), weathering grade W1. Specimens: type specimen 7.4 g and irregular metal with included olivine and pyroxenes. Rare one polished mount, MNHNP; main mass Merlier. CAI amoeboids and patches of phyllosilicates are sparsely distributed throughout the matrix. Matrix olivine, Fa1.4–6.6 and Northwest Africa 3100 orthopyroxenes, Fs3.4–5.2Wo0.3–0.7. Shock stage, S2; Morocco weathering grade W1. Specimens: type specimen 12.35 g, Purchased 2003 June NAU; main mass, Oakes. Primitive achondrite A 136 g complete stone with weathered crust was purchased Northwest Africa 3106 in Rissani. Description and classification (T. Bunch and J. Morocco Wittke, NAU): polygonal-granular, fine-grained (avg. size Found 2003 0.155 mm; range, 0.03 to 0.7 mm), thoroughly recrystallized Achondrite (diogenite) (two very small relict chondrules were observed in one of two A single, 130 g complete stone was purchased in Rissani in thin sections). Mineral modes (vol%): olivine, 78; December, 2003. Description and classification (T. Bunch orthopyroxene, 10; plagioclase, 5; troilite, 5; metal, 1; and J. Wittke, NAU): brecciated, monomict diogenite with chromite, diopside and merrillite all <1; olivine is greatly subrounded clasts that range from shock level S2 to S4; enhanced and metal is depleted relative to LL6 chondrites. metal-rich (metal = 11.7 vol%). Low-Ca pyroxene shows a Olivine, Fa28.7 (FeO/MnO = 65.6; orthopyroxene, Fs23.5Wo0.8 narrow compositional range in all clasts and matrix: Fs30.0–30.7 (FeO/MnO = 48.8); plagioclase, An34.1Or3.1; diopside, Wo3.4–3.9, Fe/Mn = 23.8–26.6; plagioclase, An94.2; kamacite, Fs12.8Wo41; Ni-rich troilite, Ni = 4.2 wt%; metal (taenite Ni = 5.9 wt%; taenite, Ni = 39.9 wt%. Low weathering grade, only), Ni = 20.1 wt%; chromite, Cr/(Cr+Al) = 0.80, Mg/ slight oxidation and staining. Specimens: type specimen 20.4 (Mg+Fe) = 0.21. Shock stage, S1; weathering grade, W2. g, NAU; main mass, Oakes. Oxygen isotopes: replicate analyses of an acid-washed whole rock sample by laser fluorination (T. Larson and F. Northwest Africa 3116 Longstaffe, UWO) gave respectively δ18O = +1.54, +1.15‰, Northwest Africa δ17O = –0.92, –1.07‰, ∆17O = –1.72, –1.66‰, which imply Found 2002 that this specimen has affinities with CR chondrites (Bunch et Carbonaceous chondrite (CK5) al. 2005). Specimens: type specimens, 20.2 g, and two A 27 g stone was purchased in Erfoud, Morocco in 2002. polished thin sections, NAU; main mass, Farmer. Description and classification (T. Bunch and J. Wittke, NAU): contains numerous amoeboid and melilite-spinel-rich CAIs; Northwest Africa 3102 well-crystallized matrix of mostly fine-grained olivine Morocco (Fa35.4), plagioclase (An39.5), magnetite (Cr2O3, 2.93 wt%; Found 2003 Al2O3, 2.85 wt%; MgO, 0.65 wt%; P2O5, 0.35 wt%; TiO2, Enstatite chondrite (EL6) 0.85 wt%; NiO, 0.43 wt%; CoO, 0.26 wt%), and troilite. A single 68.2 g stone was purchased in Rissani, Morocco in Several large xenoliths of shock-melted/crystallized material June 2003. Description and classification (T. Bunch and J. contains bundles of Ca-rich pyroxene (Fs14.1Wo49.1) set in a Wittke, NAU): completely recrystallized, fine-grained groundmass of micron-size, Ca-poor pyroxenes (Fs34.2Wo2.0) (<0.6 mm diameter) assemblage of mostly enstatite and pentlandite (Ni = 36.7 wt%). Shock level, S3 (xenoliths, (En98.5Wo0.6Fs0.9) with minor plagioclase (An18.8Or5.1). S6); low weathering grade. Specimens: type specimen 5.4 g, kamacite (Ni = 6.6 wt%; Si = 1.10 wt%); Al-bearing SiO2 NAU; main mass, Hupé. phase, graphite, alabandite (Fe = 13.4 wt%; Mg = 2.37 wt%); (Fe = 0.88 wt%) and daubreelite. Complex sulfates Northwest Africa 3117 are also present and are probably terrestrial oxidation Northwest Africa products. Shock stage, S2 with low-grade weathering. Found 2003 Specimens: type specimen 13.8 g, NAU; main mass, Oakes. Achondrite (howardite) Three stones that weigh a total of 2.45 kg were purchased in Northwest Africa 3105 Erfoud, Morocco in December 2003. Description and Morocco classification (J. Wittke and T. Bunch, NAU): howardite Found 2001 breccia of fine to medium clast size (<3.0 mm); very Carbonaceous chondrite (CR2) heterogeneous distribution of diogenite clasts; cumulate A single 89.2 g stone with 80% crust was purchased in basalt clasts were probably derived from the same basaltic The Meteoritical Bulletin No. 89 A219 provenance. All clasts are highly shocked (shock level 3–6): Northwest Africa 3133 pyroxenes and plagioclase were subjected to shock-induced, Morocco solid-state recrystallization; a few have completely melted. Purchased 2004 March/August Eucrite pigeonite, Fs47.3–52Wo16.7–7.7; Ca-rich pyroxene, Primitive achondrite (ungrouped) Fs40Wo25.2, Fe/Mn = 28.5; plagioclase, An90.7–92.0; chromite, Several complete, dense, brown stones (total 2393 g) were cr# = 80.3, fe# = 94.8; metal, Ni = 1.99 wt%; ilmenite and purchased in Tagounite by a Moroccan dealer for A. and G. silica. Diogenite orthopyroxene, Fs48.4–54.9Wo1.1–2.7, Fe/Mn = Hupé (Hupé) in 2004 March and August. Classification and 32.5. Possibly paired with NWA 1929. Low weathering mineralogy (T. Bunch and J. Wittke, NAU; A. Irving and S. grade. Specimens: type specimen 3.8 g, NAU; 21.4 g, UCLA; Kuehner, UWS): equigranular texture of subhedral to anhedral main mass, Hupé. grains with ~120° triple junctions; mean grain size = 0.28 mm. Moderate but pervasive weathering (W2) has Northwest Africa 3118 converted some metal and troilite to brown iron hydroxides, Northwest Africa which also coat grain boundaries. Mineral mode in vol%: Found 2003 olivine 46, orthopyroxene 28, plagioclase 7, Cr diopside 5, Carbonaceous chondrite (CV3) Na-Mg-bearing merrillite 4, metal (including associated Hundreds of fragments (total weight of 5895 g) were hydroxides) 5, chromite 3 and troilite 2. Highly equilibrated purchased in Erfoud, Morocco in December 2003 by A. and mineral compositions: olivine (Fa22.2 to Fa22.6, FeO/MnO = G. Hupé. Description and classification (T. Bunch and J. 57–69), orthopyroxene (Fs18.6Wo2.8 to Fs19.2Wo2.1, FeO/MnO Wittke, NAU): olive-grey to tan in color depending on the = 38–49), diopside (Fs7.3Wo44.6 to Fs8.7Wo42.2, FeO/MnO = degree of weathering. In thin section, much of the matrix has 21–33, Cr2O3 = 0.56 to 0.82 wt%, Al2O3 =1.21–1.74 wt%), a pronounced “ripple” texture: subparallel, curvilinear thin plagioclase (An50.1Or2.5 to An53.5Or2.3), metal (Ni = 17.4– bands of olivine grains (Fa32–36), up to 10 µm in size, enclose 20.2 wt%), chromite (TiO2 = 2.61 wt%, Cr/(Cr+Al) = 0.73), pod-like masses of micron to submicron Fe-rich olivine troilite (Ni = 1.2–5.2 wt%). Oxygen isotopes: replicate (Fa42–58), pyroxenes, sulfides, and minor weathering analyses of an acid-washed whole rock sample by laser products. Chondrules are typically <2 mm in diameter, fluorination (D. Rumble, CIW) gave respectively δ18O = although a few chondrules may be as large as 8 mm in +3.06‰, +2.46‰; δ17O = –1.75‰, –2.25‰ and ∆17O = – diameter. Many types of small CAI inclusions are present and 3.36‰, –3.54‰. Triplicate analyses of an acid-washed rarely exceed a few mm in diameter. A small stone was found olivine-rich separate by laser fluorination (T. Larson and F. to contain a dark inclusion measuring approximately 9 cm × Longstaffe, UWO) gave respectively δ18O = +1.78‰, 2.5 cm × 1 cm. Low weathering grade: no metal observed in +0.92‰, +0.89‰; δ17O = –2.91‰, –3.67‰, –3.62‰ and the matrix, although some chondrules contain fresh metal. ∆17O = –3.84‰, –4.16‰, –4.08‰. All of these oxygen Specimens: type specimen 20.3 g, NAU; main mass, Hupé. isotope compositions plot on the CV3 mixing line, suggesting that this achondritic meteorite has affinities with CV Northwest Africa 3127 chondrites (Irving et al. 2004c). Specimens: type specimen Northwest Africa 20.1 g, and one polished thin section, NAU; 40.3 g, and four Found 2002 polished thin sections, UWS; main mass, Hupé. Ordinary chondrite (LL3.1) A 487 g stone was purchased in Safsaf, Morocco in October Northwest Africa 3134 2002. Description and classification (T. Bunch and J. Wittke, Morocco NAU; J. Grossman, USGS): polymict chondritic breccia; host Purchased 2004 March is LL3.1 with xenoliths of LL4 and LL5. Chondrules are very Enstatite chondrite (EL6) similar to the LL3.0 Semarkona and LL3.1 NWA 1756 A very fresh (W0), complete stony meteorite (970 g) with a chondrites in terms of phase and mesostasis compositions, thin, exterior weathering rind was purchased in Rissani by a zoning profiles, and textures. FeO contents in 65 type II Moroccan dealer for A. and G. Hupé (Hupé) in 2004 March. chondrule olivine cores range from 7.0 to 26.8 wt% and Classification and mineralogy (A. Irving and S. Kuehner, corresponding CaO from 0.06 to 0.20 wt%, which are UWS): this meteorite contains abundant enstatite consistent with an LL3.0–3.2 classification (Jones, 1990); (En98.6Wo1.2–En99.3Wo0.6, 0.16–0.22 wt% Al2O3) and metal Cr2O3 contents in these olivines, which is considered to be a (kamacite containing 1–2 wt% Si, and rare taenite more sensitive indicator of petrologic subtype (Grossman and inclusions) with subordinate sodic plagioclase (An9.9Or6.0– Brearley 2005), range from 0.08 wt% to 0.58 wt% with an An11.9Or4.7), troilite (titanium-poor, with rare daubreelite average of 0.38 wt%, consistent with an LL3.1 classification, blebs), alabandite, and unusually fresh oldhamite (with Chondrule mesostasis is optically isotropic and SEM images ferroan reaction rims against metal). No chondrules were show little evidence for metamorphic crystallization of observed. This specimen may be paired with NWA 3102. mesostasis glass. Shock level, S2; weathering grade is W3. Specimens: type specimens 21.7 g, and one polished thin Specimens: type specimen 20.1 g, NAU; main mass Hupé. section, UWS; 3.7 g, NAU; main mass, Hupé. A220 S. S. Russell et al.

Northwest Africa 3136 Purchased 2004 November Algeria or Morocco Primitive achondrite Purchased 2004 April A single stone weighing 678.4 g was purchased by H. Strufe Lunar meteorite (basaltic regolith breccia) (Strufe) from a Moroccan dealer in Erfoud in 2004 An oriented 95.1 g shield-shaped stone with partial thin, pale November. Classification and mineralogy (A. Irving and S. brown fusion crust found in Algeria or Morocco was Kuehner, UWS; T. Bunch, NAU): metamorphic aggregate purchased in Tagounite by a Moroccan dealer for A. and G. (average grain size 0.2 mm) consisting of olivine (Fa18.2 –18.7, Hupé (Hupé) in 2004 April. The specimen has a thin, dark FeO/MnO = 35.0–37.6), orthopyroxene (Fs16.2Wo4.0– weathering varnish, but the interior is a very fresh, black, Fs16.6Wo4.2, FeO/MnO = 24.3–25.7), plagioclase hard, vitreous-looking rock with small white to yellowish (An12.3Or6.7–An27.4Or2.8), clinopyroxene (Fs7.4Wo43.4– clasts. Classification and mineralogy (S. Kuehner and A. Fs8.5Wo40.4, FeO/MnO = 15.8–21.7) and metal (mostly Irving, UWS): Polymict breccia consisting of mineral and kamacite with 5% Ni and bands of taenite with 30% Ni, but lithic clasts derived predominantly from mare basalt and mare heavily altered to limonite) with accessory Al-poor chromite, microgabbro lithologies, and additionally some highlands merrillite, and Ni-bearing troilite. Limonite forms abundant clasts, in a very fine grained, mostly crystalline and partly veinlets throughout the sample (W2–3). This specimen is vitreous, vesicular matrix. Mineral clasts include calcic essentially identical in texture, mineral compositions and plagioclase (An86–97), pyroxenes (orthopyroxene, degree of alteration to a polished slice of NWA 2353 ferropigeonite, ferrosilite, pyroxferroite; FeO/MnO = 68.9– analyzed concurrently, and it is concluded that these are 75.8), olivine (mostly Fa30–43, but ranging to nearly pure paired stones. Both specimens are modally heterogeneous fayalite; FeO/MnO = 81.9–94.2), ilmenite, Ni-poor Fe metal, (especially with respect to chromite, clinopyroxene and troilite, Cr-bearing ulvöspinel, and rare pentlandite, merrillite), and also with respect to plagioclase composition. baddeleyite, and a Ce-Ca-Fe-bearing, Zr-rich titanate Furthermore. it is likely that both of these stones are paired (probably zirconolite). A further description can be found in with NWA 2635. Specimens: type specimen, 28.6 g, and one (Kuehner et al. 2005). Bulk compositions (R. Korotev, polished thin section, NAU; one polished mount, UWS; 201 WUSL): INAA of several subsamples indicate that this g, Hupé; main mass, Strufe. specimen is dominated by mare components with ~20% lunar highland components (Korotev and Irving 2005). Oxygen Northwest Africa 3146 isotopes (D. Rumble, CIW): analyses of two whole rock Morocco or Algeria fragments by laser fluorination gave δ18O = +5.83‰, 5.96‰, Purchased 2003 December δ17O = +3.06‰, +3.10‰, ∆17O = –0.03‰, –0.05‰, Rumuruti chondrite (R4) respectively. Specimens: type specimens, 19.5 g, two Several brown stones (total weight 304 g) were purchased polished thin sections, and one polished mount, UWS; main from a Moroccan dealer in Erfoud by A. and G. Hupé (Hupé) mass, Hupé. in 2003 December. Classification and mineralogy (A. Irving and S. Kuehner, UWS): complex genomict to polymict Northwest Africa 3143 breccia composed of sparse clasts in a matrix of similar Morocco lithologies. All components consist of relatively well-formed Purchased 2004 August chondrules of various types and some angular (possibly Achondrite (diogenite) xenocrystic) mineral clasts in a finer grained matrix. Most A complete 2335 g stone with black fusion crust and pale chondrules contain relatively ferroan, Ni-bearing olivine orange, translucent interior was purchased from a Moroccan (Fa40.3–40.5, NiO = 0.23–0.26 wt%) typical of R chondrites, dealer in Rissani by A. and G. Hupé (Hupé) in 2004 August. but some chondrules contain more magnesian olivine (~Fa20 Classification and mineralogy (A. Irving and S. Kuehner, and ~Fa2–5) or magnesian orthopyroxene (~Fs10). Other UWS): predominantly orthopyroxene (Fs24.9Wo3.3, FeO/MnO phases include Ti-bearing chromite, Cr-bearing = 34.9) with minor chromite (some as relatively large grains), clinopyroxene (Fs9.7Wo47.1 to Fs11.4Wo45.3, Cr2O3 = calcic plagioclase, olivine (Fa26.5, FeO/MnO = 40.8), troilite 0.57 wt%), relatively sodic plagioclase (An12.2Or3.6 to and altered Ni-poor metal. Partly cataclasized metamorphic An27.7Or0.9; some as large, angular grains), Cr-rich texture with ~120° triple grain junctions among orthopyroxene laths, iron sulfide, probable xenocrysts of compositionally homogeneous orthopyroxene grains. The olivine (~Fa15) and orthopyroxene (Fs12.5Wo0.3), and overall pale orange color of this sample appears to be the interstitial feldspathic glass. Specimens: type specimen, 20 g, result of mild staining by iron hydroxides. Specimens: type and one polished thin section, UWS; main mass, Hupé. specimen, 22.7 g, and one polished thin section, UWS; main mass, Hupé. Northwest Africa 3149 Morocco Northwest Africa 3145 Purchased August 2004 Morocco Achondrite (howardite) The Meteoritical Bulletin No. 89 A221

A very fresh 2594 g stone with complete black and brown Oum Dreyga 24°18′N, 13°6′W fusion crust was purchased in Ouarzazate from a Moroccan Gour Lafkah, Western Sahara dealer by A. and G. Hupé (Hupé) in 2004 August. Fell 2003 October 16, 02:00 UT Classification and mineralogy (A. Irving and S. Kuehner, Ordinary chondrite (H3–5) UWS): breccia consisting mainly of coarse-grained mineral On 16 October 2003, Moroccan soldiers stationed in Western clasts with subordinate clasts of basaltic eucrite. Mineral Sahara saw a meteorite falling on Gour Lafkah Mountains, clasts include abundant large, pale green diogenitic south of Zbayra, about 21 km from Oum Dreyga. The orthopyroxene (Fs25.3Wo2.0, FeO/MnO = 31.1), calcic meteorite fell near a 670 km long wall built in 1985, protected plagioclase, exsolved pigeonite, silica polymorph, minor by antipersonnel mines, and guarded by soldiers. About 17 kg olivine (Fa44.4, FeO/MnO = 52.9), troilite, ilmenite (one with were recovered. Stones from this fall were later brought to a baddeleyite inclusion) and metal (5% Ni). Several clasts Moroccan dealers. Most of them were collected after a consist of subhedral orthopyroxene grains within a matrix of rainfall and are thus slightly oxidized. However, some troilite and partly altered metal. Specimens: type specimen, fragments were picked up soon after the fall; these are very 20 g, and one polished thin section, UWS; main mass, Hupé. fresh. Fragments have been sold under the names Amgala and Gor Lefcah. Classification and mineralogy (M. Bourot- Northwest Africa 3171 Denise, MNHNP): very fresh, with a black fusion crust; H3–5 Algeria breccia (Fa16.7 ± 6.0; Fa19.5 ± 0.8; Fs14.4 ± 4.4; Fs17.4 ± 1.3), S4, W0. Purchased 2004 February Specimens: type specimen 20 g and two polished mounts, Martian meteorite (shergottite) MNHNP; one 1 kg complete stone and 30 fragments totalling A 506 g broken, greenish-grey stone, believed to have been 862 g, Thomas. found in western Algeria, was purchased by A. Aaronson for D. Gregory (Gregory). About half of the stone is coated by Pecora Escarpment 01003 85º41.116′S, 68º47.542′W black fusion crust with flow orientation, and in addition there Pecora Escarpment, Antarctica are some small, wart-like protrusions on several sides of the Find 2002 January 17 stone that appear to be localized concentrations of pyroxene Pallasite coated with fusion crust. Classification and mineralogy (A. A 2.7 g meteorite fragment was collected on the blue ice at the Irving and S. Kuehner, UWS; C. Herd, UAlberta): the sample Pecora escarpment by a member of the Planetary Studies consists of subequal amounts of intergrown prismatic, Foundation’s Antarctica 2002 Expedition. Classification (P. greyish-brown pyroxene and sparkling, glassy maskelynite. Sipiera, PSF): upon close examination the meteorite was Pyroxenes are zoned from cores of subcalcic augite determined to be a fragment of a pallasite. It clearly exhibits (Fs19.3Wo33.1, FeO/MnO = 26.4) and pigeonite (Fs29.9Wo12.1, surface characteristics indicating where olivine had FeO/MnO = 28.2) to pigeonite rims as ferroan as Fs72.9Wo9.8 weathered away. No olivine grains were present for analysis, (FeO/MnO = 39.9). Plagioclase has been converted entirely to and the small size and rough nature of the specimen did not maskelynite and is compositionally inhomogeneous make microprobe analysis possible without destroying the (An41.5Or3.7–An54.4Or1.3). Accessory phases are ulvöspinel, specimen. Specimens: type specimen, 2.7 g DuPont. ilmenite, chlorapatite, Na-K-Al-Si-rich glass, silica (formerly stishovite, judging from radial cracks around some grains), Pecora Escarpment 01006 85º41.011′S, 68º48.045′W merrillite, pyrrhotite and baddeleyite. Rare barite and calcite Pecora Escarpment, Antarctica probably are products of minor desert weathering. Minor Find 2002 January 17 rusty staining around ulvöspinel grains and along thin, black Enstatite chondrite (E4) fractures appears to be a complex mixture of fine-grained iron A 0.75 g meteorite was collected on the blue ice at Pecora hydroxide and Si-Al-Ca-Mg-Cl-K-bearing phases, and Escarpment by a member of the Planetary Studies possibly is a product of pre-terrestrial alteration (Irving et al. Foundation’s Antarctica 2002 Expedition. Classification (P. 2004a). This specimen is not obviously paired with any of the Sipiera, PSF): the probe section was dominated by pyroxene other four African olivine-free basaltic shergottites (Zagami, and no olivine was present. The pyroxene analyses gave a NWA 480, NWA 856 or NWA 1669). Oxygen isotopes (T. mean composition of En97.58Fs1.49Wo0.93 (n = 28). The Si Larson and F. Longstaffe, UWO): pyroxene δ18O = +4.43 ± content in the metal was determined to be 1.5 wt%. The 0.06‰, δ17O = +2.72 ± 0.00‰, ∆17O = +0.42 ± 0.03‰; petrologic type was determined petrographically. Specimens: maskelynite δ18O = +4.69 ± 0.07‰, δ17O = +2.82 ± 0.1‰, type specimen, 0.75 g DuPont. ∆17O = +0.38 ± 0.07‰. Specimens: type specimen, 22 g and four polished thin sections, UWS; main mass, Gregory. Podgrodzie 50°54.20′N, 21°32.99′E Poland, åwiÍtokrzyskie province, Tarnobrzeg county Ordinary Chondrite Finds from Eurasia Found 2000 March Table 8 lists 8 ordinary chondrite meteorites that were found Ordinary chondrite (H4/5) in various locations in Eurasia. An 8.9 g stone was recovered in a gravel pit (4 m below A222 S. S. Russell et al. surface) of quaternary sediments by Pawe≥ Osowski using a wt% CaO in FeO-poor chondrules. Weathering grade is W2/3 metal detector. It has been broken in many small fragments (metal is oxidized, sulfide almost intact). Specimens: type (max. 3 g) and splinters. Classification and analysis (R. specimen 30.2 g and one polished mount, MNHNP; main Bartoschewitz, Bart; P. Appel and B. Mader, Kiel): olivine mass with Annick Goueslain and Jean Luc Parodi. Fa18.7 ± 0.3; low-Ca pyroxene Fs16.4 ± 0.2Wo1.3 ± 0.3; Ca-rich pyroxene Fs28.2Wo25.7; troilite Ni 0.48%, Co 0.11%. Cr Tanezrouft 087 25°45.366′N, 00°16.075′E 0.03%. Shock stage S1, weathering grade W2. Magnetic Algeria, east Tanezrouft susceptibility: logχ = 5.14 × 10–9 m3/kg; Specimens: type Found 2003 December 23 specimen, 1.76 g KrakÛw; 4.2 g and polished thin section, Ordinary chondrite (H5) Bart; 3 g P. Osowski, BodzentyÒska 44, PL-25-308 Kielce. One 320 g stone, partially covered with a reddened fusion crust was found. Classification and mineralogy (M. Bourot- Rahimyar Khan 28°13.5′N, 70°12′E Denise, MNHNP): the stone is an H5 with a large clast of CO3 Rahimyar Khan, Pakistan material comprising about 30% of the entire mass. Host Fell 1983 December lithology: olivine, Fa20.6 ± 0.2; low Ca pyroxene, Fs18.0 ± 0.3; the Ordinary chondrite (L5) chondritic texture is still clearly visible, with many chondrule A few shepherds heard thundering sounds and later found a relics. Shock stage S2, weathering grade W3. CO3 clast: it is single 67.225 kg stone buried about 1 m deep in a sand dune. much more altered, most metal grains are oxidized and Classification (A. Rubin, UCLA): the meteorite is a chondrite; silicates are reddened; chondrules are small (~100 µm) and Fa23.5, S3, W1. Specimens: type specimen 25 g UCLA; main set in a fine-grained matrix with abundant small sulfide mass anonymous. grains. Opaque nodules comprise rusted metal, sulfide and magnetite. Estimated metamorphic grade between those of Ramlat as Sahmah—Correction Colony and Kainsaz. Olivine, Fa1.6–32.6, mean Fa15.3 ± 7.5, up to The name “Ramadah as Sahmah” appears in previous 0.4 wt% CaO; pyroxene, Fs2.0–18.4, mean Fs10.1 ± 5.5. bulletins and this is incorrect. The correct region name is Specimens: type specimen 35.1 g and one polished mount, Ramlat as Sahmah. Meteorites from this region will MNHNP; main mass with Annick Goueslain and Jean Luc henceforth have this name, meteorites previously named will Parodi. have a synonym of Ramlat as Sahmah XXX. Tiffa 008 20°21.500′N, 11°51.000′E San Michele 43°40′N, 13°00′E Niger Pesaro Urbino, Marche, Italy Found 2001 October Fell 2002 February 20, 06:45 local time Carbonaceous chondrite (CO3) Ordinary chondrite (L6) A single brown stone of 1149 g was found by G. Moreau in Miss Raffaela Frezzotti was woken up by a sound coming the Ténéré desert. The fusion crust is well preserved and from the roof of her house. Two days later she found a hole in covers 90% of the external surface of the stone. Mineralogy the roof of her house and a single black 237 g stone in the loft. and classification (E. Dransart, EMTT): chondrule mean size Classification (A. Maras, URoma): the stone is an ordinary 0.185 mm; many refractory inclusions; mean olivine chondrite, Fa25.4, Fs21.6; weathering grade W0. Specimens: composition Fa26.7 (range Fa0.18–37.9); low-Ca pyroxene mean type specimen, 52 g Museum of Mineralogy, URoma, main composition Fs8.2 (range Fs3.4–45.1). Shock stage S2; mass (181 g), finder. weathering grade W1. Specimens: type specimen, 22.2 g MNHNP; main mass, Gabelica. Tanezrouft 082 24°49.036′N, 00°26.057′W Algeria, west Tanezrouft Uruq al Hadd 001–002—Correction Found 20 December 2003 The locality name for these two meteorites was misspelled in Carbonaceous chondrite (CM2) Table 5 of The Meteoritical Bulletin No. 88. The correct A single, completely crusted stone, weighing 1012 g, was spelling is “Uruq al Hadd.” found. Crust has polygonal cracks (terrestrial alteration), interior is black and slightly friable. Classification and Verkhnyi Saltov 50°06.667′ N, 36°48.006′ E mineralogy (M. Bourot-Denise, MNHNP): small, typically Kharkov district, Ukraine <100 µm with few in the 300–800 µm size range, rounded Found 2001 April or May chondrules, abundant angular debris and a few CAIs are set in Iron, coarse octahedrite (IIIAB) a very dark matrix. Matrix contains troilite, pentlandite and An iron (21 × 16 × 7 cm) weighing 9.53 kg was found during clusters of framboidal magnetite. Olivine, Fa0.44–64.4, mean archeological work at the shoreline of the Pechenezhsky Fa14.5 ± 17.0; orthopyroxene, Fs0.92–14.9, mean Fs2.5. Olivines water reservoir, 2 km south of the Verkhnyi Saltov village. are zoned in FeO-rich chondrules, they contain up to 0.54 This piece was recovered within the Verkhnesaltov The Meteoritical Bulletin No. 89 A223 archeological complex. This site used to be a large capital city Kuehner S. M., Irving A. J., Rumble D., III, Hupé A. C., and Hupé of the Khazar state between the 8th and 10th centuries. G. M. 2005. Mineralogy and petrology of lunar meteorite NWA Classification and mineralogy (M. A. Nazarov, Vernad.): the 3136: A glass-welded mare regolith breccia of mixed heritage (abstract #1228). 36th Lunar and Planetary Science Conference. piece was enveloped by Fe hydroxide layer of about 5 mm CD-ROM. thick; kamacite (5.9–6.8 wt% Ni; 0.48–0.59 wt% Co) and Lauretta D. S. Killgore M. Greenwood R. C. Verchovsky A. B., and taenite (25.7–30.8 wt% Ni; 0.17–0.34 wt% Co) form the Franchi I. A. 2004. The Fountain Hills meteorite: A new CBa Widmanstätten pattern with 1.5–3 mm kamacite bandwidths; chondrite from Arizona (abstract #1255). 35th Lunar and rare troilite-chromite inclusions are present. INAA data (J. T. Planetary Science Conference. CD-ROM. La Blue A. R., Lauretta D. S., and Killgore M. 2004. Chondrules and Wasson, UCLA): Ni 79.5, Co 4.99 (mg/g), Cr 42, Cu 146, Ga isolated grains in the Fountain Hills bencubbinites (abstract 20.7, Ge <41, As 4.99, Ru 8.5, Re 0.258, Ir 3.16, Pt 10.0, Au #9063). Workshop on Chondrites and the Protoplanetary Disk. 0.682 (µg/g) indicate the IIIAB group. Specimens: type Mittlefehldt D. W., McCoy T. J., Goodrich C. A., and Kracher A. specimen 1.03 kg, Vernad; main mass with anonymous 1998. Non-chondritic meteorites from asteroidal bodies. In owner. Planetary materials, edited by Papike J. J. Washington D.C: Mineralogical Society of America. Oberst J., Heinlein D., Köhler U., and Spurn˝ P. 2004. The multiple Acknowledgments–This Bulletin was prepared by the meteorite fall of Neuschwanstein: Circumstances of the event Meteorite Nomenclature Committee of the Meteoritical and meteorite search campaigns. Meteoritics & Planetary Society under the Principal Editorship of Sara Russell. Science 39:1627–1642. Members for 2005 are: H. Chennaoui, H. C. Connolly Jr. Promprated P., Taylor L. A., Anand M., Rumble III D., Korochantseva E. V., Ivanova M. A., Lorentz C. A., and Nazarov (Associate Editor for Oman), L. Folco (Associate Editor for M. A. 2003. Petrology and oxygen isotopic compositions of Africa), J. Goldstein, J. Goswami, M. Grady, J. Grossman, R. anomalous NWA 011 (abstract #1757). 34th Lunar and Planetary Jones (Associate Editor for the Americas), Y. Lin, K. Righter Science Conference. CD-ROM. (Associate Editor for Antarctica), M. Nazarov, A. Yamaguchi, Stöffler D., Keil K. and Scott E. R. D. 1991. Shock metamorphism of J. Zipfel (Chair 2005) and M. Zolensky (Associate Editor for ordinary chondrites. Geochimica et Cosmochimica Acta 55: 3845–3867. Northwest Africa). Warren P. H. 2005. “New” lunar meteorites: Implications for composition of the global lunar surface, lunar crust, and the bulk REFERENCES Moon. Meteoritics & Planetary Science 40:477–490. Wasson J. T. and Kallemeyn G. W. 2002. The IAB iron-meteorite Clayton R. N. and Mayeda T. K. 1999. Oxygen isotope studies of complex: A group, five sub-groups, numerous grouplets, closely carbonaceous chondrites. Geochimica et Cosmochimica Acta 63: related, mainly formed by crystal segregation in rapidly cooling 2089–2104. melts. Geochimica et Cosmochimica Acta 66:2445–2473. Bunch T. E., Irving A. J., Larson T. E., Longstaffe F. J., Rumble D., III, Wlotzka F. 1993. A weathering scale for the ordinary chondrites and Wittke J. H. 2005. “Primitive” and igneous related (abstract). Meteoritics 28:460. to the large and differentiated CR (abstract #2308). Yamaguchi A., Clayton R. N., Mayeda T., Ebihara M., Oura Y., Miura 36th Lunar and Planetary Science Conference. CD-ROM. Y. N., Haramura H., Misawa K., Kojima H., and Nagao K. 2002. Grossman J. N. and Brearley A. J. 2005. The onset of metamorphism A new source of basaltic meteorites inferred from Northwest in ordinary and carbonaceous chondrites. Meteoritics & Africa 011. Science 296:334–336. Planetary Science 40:87–122. Irving A. J., Herd C. D. K., Kuehner S. M., Gregory D. A., and ABBREVIATIONS FOR ANALYSTS AND SPECIMEN Aaronson A. A. 2004a. Petrology and redox state of basaltic LOCATIONS shergottite NWA 3171 (abstract). Meteoritics & Planetary Science 39:A49. Irving A. J., Bunch T. E., Kuehner S. M., and Wittke J. H. 2004b. These abbreviations are used in the “Info” columns of tables Petrology of primitive olivine-orthopyroxene-phyric shergottites in The Meteoritical Bulletin. Unless stated otherwise, type NWA 2046 and NWA 1195: Analogies with terrestrial boninites specimen is at the analyst’s institution and the main mass is and implications for partial melting of hydrous Martian mantle (abstract #1444). 35th Lunar and Planetary Science Conference. with the finder. CD-ROM. Irving A. J., Larson T. E., Longstaffe F. J., Rumble D., Bunch T. E., Asu1: classified by G. Huss, ASU. Wittke J. H., and Kuehner S. M. 2004c. A primitive achondrite Asu2: classified by L. Bleacher, ASU; main mass, finders I. with oxygen isotopic affinities to CV chondrites: Implications for and A. Nelson. differentiation and size of the CV parent body (abstract #P31C- 02). Eos Transactions 85. Asu3: classified by G. Huss, ASU; main mass, finder M. Irving A. J., Bunch T. E., Wittke J. H., and Kuehner S. M. 2005. Wolff; type specimen, Denver. Olivine-orthopyroxene-phyric shergottites NWA 2626 and DaG Asu4: classified by G. Huss, ASU; finder, K. Jarnagin; main 476: The Tharsis connection (abstract #1229). 36th Lunar and mass and type specimen, Denver. Planetary Science Conference. CD-ROM. Asu5: classified by G. Huss, ASU; main mass, M. Brown. Korotev R. L. and Irving A. J. 2005. Compositions of three lunar meteorites, Meteorite Hills 01210, Northeast Africa 001, and Asu6: classified by G. Huss, ASU; main mass, finder, J. R. Northwest Africa 3136 (abstract #1220). 36th Lunar and Williams. Planetary Science Conference. CD-ROM. Asu7: classified by G. Huss, ASU; finder, A. T. Beckman; A224 S. S. Russell et al. main mass and type specimen, Denver. La1: classified by J. T. Wasson, UCLA; main mass Birdsell. Asu8: classified by G. Huss, ASU; finder, K. Rothrock; main La2: classified by A. Rubin, UCLA; finder, D. Brookins; main mass and type specimen, Denver. mass, Kansas Meteorite Society. Bart1: classified R. Bartoschewitz, Bart, P. Appel and B. La3: classified by A. Rubin, UCLA; finder, John Wolfe; main Madar, Keil; type specimen Krakov. mass, Verish. Bart2: classified R. Bartoschewitz, Bart, type specimen La4: classified by A. Rubin, UCLA; main mass, finder Verish. Vernadsky Institute; specimen Bart, main mass Flemming/ La5: classified by A. Rubin, UCLA; main mass, finder N. Berlin. Gessler. Bart3: classified R. Bartoschewitz, Bart, type specimen La6: classified by A. Rubin, UCLA; main mass, finder P. Vernadsky Institute; specimen Bart, main mass EgerBe2: Gessler. classified by A. Greshake, MNB and M. Kurz. La7: classified by A. Rubin, UCLA; finder G. LaBarbera; Be3: classified by A. Greshake, MNB and M. Kurz; oxygen main mass, Verish. isotopes, I. A. Franchi and R. Greenwood, OU. La8: classified by A. Rubin, UCLA; finder J. LaBarbera; main Be5: classified by A. Greshake, MNB; main mass, Stefan mass, Verish. Ralew, Kunibertstrasse 29, 12524 Berlin. La9: classified by A. Rubin, UCLA; main mass, finder T. Be6: classified by A. Greshake, MNB; main mass, Peter Kunihiro. Marmet, Bern, Switzerland. La10: classified by A. Rubin, UCLA; finder, D. Thomas; type Be7: classified by A. Greshake, MNB and M. Kurz; main specimen, PSF; main mass, Verish. mass, C. Anger, Austria. La11: classified by A. Rubin, UCLA; finder, G. Long; type Be8: classified by A. Greshake, MNB; main mass, JNMC. specimen, PSF; main mass, Verish. Ca1: classified by M. Hutson, Cascadia; finder, L. Sloan; La12: classified by A. Rubin, UCLA; main mass, finder R. type specimen, Cascadia; main mass, E. Thompson. Matson. Ca2: classified by M. Hutson, Cascadia; type specimen, La13: classified by A. Rubin, UCLA, type specimen, PSF; Cascadia; main mass, finder, J. Adams. main mass, Verish. Ca3: 1998g stone found by Homer Stockam, 03/11/2004; La14: classified by A. Rubin, UCLA, main mass, finder, C. classified by M. Hutson, ASU; main mass, L. Sloan; type Donnelly. specimen, Cascadia Meteorite Laboratory. 7160 g stone found La15: classified by P. Warren, UCLA, main mass, finder, by Sonny Clary 02/16/2004; classified by L. Bleacher and M. Labenne. Hutson, ASU. Mainz1: Data collated by J. Zipfel (Mainz) from various CAS: classified by B. Miao, Y. Lin, R. Lu and D. Wang, CAS. sources. ENSL2: classified by E.-M. Chamorro, K. Pistre, P. Beck, MK2: Classified by Marvin Killgore, Main mass Southwest ENSL, P. Grandjean, UCBL; main mass, F. Beroud (Lyon) and Meteorite Collection; type specimen at the University of C. Boucher (Chatel-Guyon). Arizona. FSAC1: classified by H.Chennaoui Aoudjehane, UHAC, M. Mün2: classified by A. Sokol, A. Bischoff and M. Niemeier, Denise, MNHNP, A. Jambon, UPVI; type specimen, UHAC; Mün, (data ± 1 mol%; EDS analyses); main mass with finder, main mass: L. Baidder (Maroc). J. Wassmann. FSAC2: classified by H.Chennaoui Aoudjehane, UHAC, M. Mün3: classified by A. Sokol, A. Bischoff, Mün, (data ± Denise, MNHNP, A. Jambon, UPVI; type specimen, UHAC; 1 mol%; EDS analyses). main mass: anonymous finder. Mün5: classified by A. Sokol, A. Bischoff, Mün; type FSAC3: classified by H.Chennaoui Aoudjehane, UHAC, M. specimens, Ham, Mün, and Mainz; main mass, Industrial Denise, MNHNP, A. Jambon, UPVI; type specimen, UHAC; Research Center (IRC) Tripoli. main mass: Bouabdellah/Chaieb/Milhi Service géologique Mün6: classified by M. Niemeier, A. Bischoff, Mün. d’Oujda Maroc. Mün7: classified by A. Bischoff, A. Sokol, M. Niemeier, Ha1: classified by P. Sipiera, PSF; main mass, Huss. Mün. Ha2: classified by P. Sipiera and K. J. Cole, PSF; oxygen Mün8: classified by A. Bischoff, A. Sokol, M. Niemeier, isotope analyses, I. A. Franchi, OU; main mass, finder Mün; main mass, JNMC. Pelisson. Mün9: classified by A. Bischoff, A. Sokol, M. Niemeier; Ha3: classified by P. Sipiera, PSF. main mass with SDCMC. Ha4: classified by P. Siperia, PSF; main mass, finder, M. Mün10: classified by A. Bischoff, A. Sokol, M. Niemeier Miller. Mün; main mass, HSSH. Ha5: classified by P. Sipiera, PSF; main mass, finder, Verish. NAU1: classified by Ted Bunch, NAU; type specimen NAU. Ha6: classified by P. Sipiera, PSF; main mass and type NAU2: classified by Ted Bunch, NAU; type specimen NAU; specimen, DuPont. main mass, Drummond. Ham1: classified by J. Schlüter, Ham; main mass, H. Burkard, NAU3: classified by Ted Bunch, NAU; type specimen NAU; Bonn and I. Herkstroeter, Hamburg. main mass, Regelman. The Meteoritical Bulletin No. 89 A225

NAU4: classified by Ted Bunch, NAU; type specimen NAU; Silesia1: classified by £ukasz Karwowski, Silesia; type main mass, Burkhard. specimens 100 g, Silesia; 57.6 g Mün; main mass, finder, NAU5: classified by Ted Bunch, NAU; type specimen NAU; Labenne. main mass, Birdsell. Sn1: classified by A. Burroni and L. Folco, MNA-SI; NAU6: classified by Ted Bunch, NAU; type specimen NAU; magnetic classification, P. Rochette, CEREGE and L. Folco main mass, Reed. MNA-SI according to Rochette et al. (2003). NAU7: classified by Ted Bunch, NAU; type specimen NAU; Sn3: classified by L. Folco, MNA-SI. main mass, Hupé. Sn4: classified by L. Folco, MNA-SI; thin section, MNA-SI; NAU8: classified by Ted Bunch, NAU; type specimen NAU; type specimen, OAM. main mass, Strufe. Sn5: classified by L. Folco, MNA-SI and M. D’Orazio, Pisa; NHMV1: classified by F. Brandstätter, NHMV; main mass, finder, F. Merighi; type specimen, OAM; 2.7 g and 3 thin finder, M. Kriegler. sections, MNA-SI. NHMV2: classified by F. Brandstätter, NHMV. TCU1: classified by A. Ehlmann, TCU and T. J. McCoy, SI; NHMV3: classified by F. Brandstätter, NHMV; main mass, finder, P. Alastuey; main mass and type specimen, TCU. finder, V. Apolloner. UAriz1: classified by D. Schrader and D. Kring, UAriz; NU: classified by H. Wang, Y. Liang, R. Wang, J. Ji, W. finder, H. McCormick; main mass, Fleischman Planetarium, Zhang and X. Chen, NU. Reno, NV. Pa1: classified by M. Bourot-Denise MNHNP; main mass, F. UCLA: classified by A. Rubin, type specimen UCLA. Kuntz and F.-X. Flotterer. UPB1: classified by B. Devouard, UBP, M. Messaoudi, H. Pa2: classified by M. Bourot-Denise, MNHNP; main mass, G. Afalfiz and D. Belhai, USTHB; type specimen, MNHNP, main Merlier. mass, M. Franco, Caillou Noir. Pa3: classified by M. Bourot-Denise, MNHNP; main mass, UPMCPa3: classified by A. Jambon, D. Badia, O. Boudouma, Labenne. UPMCP, and M. Bourot-Denise, MNHNP; main mass, finder, Pa4: classified by M. Bourot-Denise, MNHNP; main mass, B. M. Franco, Caillou Noir. Fectay and K. Bidaut. USA5: classified by M. Hutson, Cascadia; finder, L. Sloan; Pa16: classified by M. Bourot-Denise, MNHNP; main mass, type specimen, Cascadia; main mass, E. Thompson. A. Goueslain and J. L. Parodi. USA7: classified by M. Hutson, Cascadia; type specimen, Pa17: classified: M. Bourot-Denise, MNHNP; main mass, Cascadia; main mass, finder, J. Adams. Thomas. UWS1: classified by A. Irving, UWS; main mass, Hupé. Pa20: classified by M. Bourot-Denise, MNHNP; main mass, Vr1: classified by S. Afansiev, Vernad, analyzed by N. M. Franco, Caillou Noir. Kononkova, Vernad. Pa21: classified by E. Dransart, EMTT; finder G. Moreau; Vr2: classified by S. Afansiev, Vernad, analyzed by A. type specimen, MNHNP; main mass, Z. Gabelica. Ulianov, MSU. Pa22: classified by E. Dransart and M. Baron EMTT; finder G. Vr3: classified by Lorenz C.A. Vernad. Moreau; type specimen, MNHNP; main mass EMTT, finder. Vr5: classified by M. Ivanova, Vernad. Pa23: classified by M. Bourot-Denise, MNHNP; main mass, Vr6: classified by D. Badyukov, Vernad. J. L. Leran. Vr7: classified by M. Ivanova, Vernad; main mass lost. PCU1: Classified by J. Haloda and P. Tycova, PCU; type Vr8: classified by M. Nazarov, Vernad; main mass, V. specimen PCU. Anoshin. Pd1: classified by A. M. Fioretti and R. Carampin, UPad; Vr9: classified by M. Nazarov, Vernad; main mass, S. main mass and thin section, MNA-SI. Murashova and S. Murashov. Pol: Classified by £ukasz Karwowski, University of Silesia; Vr10: classified by M. Ivanova, Vernad; finder, S. Egorov. type specimen at University of Silesia. Vr11: A fireball was seen in this area in 1954, and this Prato1: classified by G. Pratesi and V. Moggi Cecchi, MSP. meteorite was found during ploughing. The meteorite was Prato2: classified by G. Pratesi and V. Moggi Cecchi, MSP; strongly heated in a forge. Classified by L. V. Agafonov, S. M. finder, G. Pratesi, MSP. Kuznetsov, L. N. Pospelova, United Institute of Geology, Prato3: classified by V. Moggi Cecchi, MSP Geophysics and Mineralogy, Novosibirsk. Main mass, Prato4: classified by V. Moggi Cecchi, MSP; main mass, Kosikhino museum, Altai District. Chinellato. Vr12: classified M. Ivanova and E. Zhiganova, Vernad; main Prato5: classified by G. Pratesi and V. Moggi Cecchi, MSP; mass, D. Kalinin. found by a hiker; main mass, Chinellato. Vr13: classified by M. Nazarov, Vernad and Th. Ntaflos, Rm1: classified by M. Macrì, A. Maras and M. Serracino, Vienna. Roma; main mass and thin section, MNA-SI. Vr14: classified by R. Batoschewitz (Bart) and P. Appel Univ. SAm1: classified by M. Valenzuela, Chile; main mass, finder, Kiel, Type specimen Vernad; Main mass Th. Kurtz, Hanover; E. Stucken. specimen Bartoschewitz. A226 S. S. Russell et al.

ADDRESSES OF METEORITE COLLECTIONS AND Kurz: M. Kurz, Schillerstrasse 7, D-34626 Neukirchen, RESEARCH FACILITIES Germany. Mainz: Institut für Chemie, Abteilung Kosmochemie, ASU: Center for Meteorite Studies, Department of Geological Postfach 3060, D-55020 Mainz, Germany. Sciences, Arizona State University, Tempe, Arizona, USA. Matson: Rob Matson, 8 Merano Ct., Newport Coast, CA Bart: Bartoschewitz Meteorite Laboratory, Lehmweg 53, D- 92657, USA. 38518 Gifhorn, Germany. MNA-SI: Museo Nazionale dell’Antartide, Università di Birdsell: Arizona Skies Meteorites, Tucson, Arizona. Siena, Via Laterina 8, I-53100 Siena, Italy. Burkard: Horst Burkard, Bonn, Germany. MNB: Museum für Naturkunde, Invalidenstrasse 43, D-10115 CAS: Chinese Academy of Sciences, Beijing, China. Berlin, Germany. Cascadia: Cascadia Meteorite Laboratory, Portland State MNHNP: Museum National d’Histoire Naturelle, Paris, University, Department of Geology, Room 17 Cramer Hall, France. 1721 SW Broadway, Portland, OR 97201, USA. MSP: Museo di Scienze Planetarie, Via Galcianese, 20/h, CEREGE: CEREGE ARBOIS, BP 80, Aix En Provence, 59100 Prato, Italy. Cedex 4, France. MSU: Moscow State University, Department of Geology, Chile: Plaza Ercilla 803, University of Chile, Casilla 13518- Vorobjovy Gory, Moscow, 119899, Russia. Correo 21, Santiago-Chile. Mün: Institut für Planetologie, Wilhelm-Klemm-Str. 10, CIW: Carnegie Insitution Washington, Geophysical 48149 Münster, Germany. Laboratory, 5251 Broad Branch Rd., NW, Washington DC NAU: Northern Arizona University, Flagstaff, AZ 86011, 20015, USA. USA. See http://www4.nau.edu/meteorite. CNRST: Centre National de Recherche Scientifique et NHM: Department of Mineralogy, The Natural History Technique, Casablanca, Morocco. Museum, Cromwell Road, London SW7 5BD, UK. Denver: Denver Museum of Natural History, City Park, NHMV: Naturhistorisches Museum, Postfach 417, A-1014 Denver, CO 80205, USA. Wien, Austria. DuPont: James M. DuPont Meteorite Collection, Planetary NMB: Museum fuer Naturkunde, Institut fuer Mineralogie, Studies Foundation 612 Chatham Circle, Algonquin, IL Humboldt-Universitaet zu Berlin, Invalidenstrasse 43, 10115 60102, USA. Berlin, Gerrmany. EMTT: Etudes Métallurgiques et de Traitement Thermique, NU: Nanjing University of Science and Technology, 1 Parc du Chater-Bât. B, 1, avenue du Chater, 69340 Lianhecun, Xiaowei Road, Nanjing, China. Francheville, France. Oakes: Nelson Oakes, Route 1, House 50C, Uniondale, PA ENSL: Ecole Normale Supérieure de Lyon, Laboratoire de 18470, USA. Sciences de la Terre, 46 allée d’Italie 69364 Lyon Cedex, OAM: Osservatorio Astronomico e Museo “Giorgio Abetti” France. in San Giovanni in Persiceto, Bologna, Italy. Farmer: Michael Farmer 4201 W. Oxbow Mine Ct. Tucson, OU: Planetary and Space Sciences Research Institute, The Arizona, USA. Open University, Milton Keynes, MK7 6AA, UK. Fectay: Bruno Fectay and Carine Bidaut, La Memoire de la UPad: Istituto di Geoscienze e Georisorse-CNR, Università Terre SARL Rue de la Mairie, 39240 La Boissiere, France. di Padova, Italy. Franco: Caillou Noir, 100 Chemin des Campènes 74400 Les PCU: Charles University, Faculty of Science, Institute for Praz de Chamonix, France. Cheochemistry, Mineralogy and Mineral Resources, Albertov Gabelica: Z. Gabelica, Université de Haute Alsace, 3 Rue A. 6, 128 43 Prague 2, Czech Republic. Werner, F-68093 Mulhouse, Cedex, France. Pelisson: Richard and Roland Pelisson, 270 Rue de la Gessler: Mr. Nicholas Gessler, Box 706, 22148 Monte Vista Cascade, 38660 La Terrasse, France. Road, Topanga, CA 90290–0706, USA. PSF: Planetary Studies Foundation, Harper College, Schmitt Gregory: David Gregory, 230 First Avenue, Suite 108, St. Meteorite Research Group, 1200 W. Algonquin Rd., Palatine, Thomas, Ontario N5R 4P5, Canada. IL 60067, USA. GSI: Geological Survey of India, 27 Jawaharlal Nehru Road, Reed: PO Box 1141, Delta, Colorado, USA. Kolkata 700016, India. ROM: Royal Ontario Museum, 100 Queen's Park, Toronto, Ham: Mineralogical Museum, Universität Hamburg, Ontario M5S 2C6, Canada. Grindelallee 48, D-20146 Hamburg, Germany. SI: Department of Mineral Sciences, NHB-119, National Hupé: G. and A. Hupé, 2616 Lake Youngs Court SE, Renton, Museum of Natural History, Smithsonian Institution, WA 98058, USA. Washington, DC 20560, USA. Köln: Universität zu Köln, Institut für Mineralogie und SML: M. Killgore, Southwestern Meteorite Laboratory, PO Geochemie, Zülpicher Strasse 49 b, 50674 Köln, Germany. Box 95, Payson, AZ 85547, USA. Krakov: Muzeum Geologiczne ING PAN, ul. Senacka 1–3, TCU: Oscar E. Monnig Collection, Dept. of Geology, Texas PL-31–002, KrakÛw, Poland. Christian University, Ft. Worth, Texas 76129. The Meteoritical Bulletin No. 89 A227

UAriz: Lunar & Planetary Laboratory, University of Arizona, Uppsala, SE-752 36 Sweden. 1629 E. University Blvd., Tucson, AZ 85721, USA. UPVI: Université Pierre & Marie Curie (Paris VI), 4 Place UBP: Université Blaise Pascal, Clermont-Ferrand, France. Jussieu, 75005 Paris, France. UCB: Université Claude Bernard, Lyon 1, France. URoma: DST, Università “La Sapienza”-Roma, Italy. UChi: University of Chicago, Chicago, IL 60637, USA. UWO: University of Western Ontario, London, Ontario N6A UCLA: Institute of Geophysics & Planetary Physics, 3KT, Canada. University of California, Los Angeles, CA 90095–1567, UWS: University of Washington, Department of Geological USA. Sciences, Box 351310, Seattle, WA 98195, USA. UHAC: Université Hassan II Aïn Chock, Faculté des Verish: Robert Verish, Meteorite Recovery Foundation, P. O. Sciences, Département de Géologie, BP 5366 Maârif Box 237, Sunland, CA 91040, USA. Casablanca Morocco. Vernad: Vernadsky Institute of Geochemistry and Analytical UJM: Universitè Jean Monnet, Saint-Etienne, France. Chemistry, Russian Academy of Sciences, Kosygin Str. 19, UMo: Department of Earth Sciences, Universiy of Modena, Moscow 117975, Russia. Modena, Italy. Vienna: University of Vienna, Dr-Karl-Lueger-Ring 1, A- UO: Université d’Oran, Es-Sénia, Algeria. 1010 Wien, Austria. Uppsala: Department of Earth Science Uppsala University, A228 S. S. Russell et al. 20.7 Be3 25.5 Mün5 26.3 Mün5 23 Ha1 14 ENSL2 10 Pa23 32.1 Pa22 720 Prato1 656 Sn3 ~350 UHAC Type spec (g) Info § a entry cv el Atchane cv paired with DaG 749, 858, 1006 entry breccia Agades entry 114Ha2 entry 13.9 (1.2–72.1) Fs (mol%) Comments (1.4-39.1) Fa (mol%) 325 1 H5/6 S5 W3 19.5 16.7 – 35.7 NHMV3 132 1 L4 S1 W1 23.8 20.1 – 167 Prato1 Mass (g) Pieces Class Shock WG E 209 5 L6 S4 W3–4 25.5 21 terrestrial sv, E 2197 Many L5/6 S3 W3 25 20.5 Terrestrial E 38000 Many H5 – – – – See separate ′ ′ ′ E 151 1 LL6 – A 30.4 25.6 3 0.4 Mainz1 E 85 1 H4 – C 18.5 15.8 2 3.7 Mainz1 E 781 15 CV3 Low Mod 19.6 (2–30) 2–7separate See E 4570.2 14 L6 S1 W2 25.4 ± 0.2 22.9 ± 1.7 20.3 Pa16 E 889 Several L6 S4 W2 22.2 18.8 sv 21 Be2 E 131 1 CO3 W2 1–65 1–32 Probably E 137 3 L5 S3 W2 25.7 24.3 – 29 Ha1 E 214 1 L3 S2 W4 ± 8.6 23.8 26.0 ± 13.7 – 43 Ha1 E 20.1 1 H5 S3 W1 18.6 ± 0.9 17.1 ± 1.2 North of ′ ′ ′ ′ ′ ′ ′ ′′ ′′ E 1272 25 H6 S2 W2 18.9 16.7 – 1272 Prato1 E 720 3 H5 S2 W3 18.1 16.2 Hammadet E 1456 1 L5 S3 W3 24.8 20.5 – 1455 Prato1 E 410 1 H5 S1 W1 19.6 17.1 – 410 Prato1 E 126 1 H4 S2 W1 19.4 17 – 125 Prato1 E 122 1 H4 – – 19.4 16.7 – 122 Prato1 E 9608 1 L5 S4 W0 23.7 20.2 – 9586 Prato1 E 238 1 LL6 – – 27.9 23.3 – 233 Prato1 E 128 1 H5 – – 18.7 16.6 – 128 Prato1 E 495 1 LL6 – – 28.7 24.2 – 495 Prato1 E 132 1 H6 – – 18.8 16.6 – 130 Prato1 E 69 1 CR2 – – 7.5 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ W kg 25–30 Many LL6 S3/4 W0 29 ± 1 25 ± 1separate See E 94 1 L4 – C 18.9 – – 94 Mainz1 26 38 ′ ′ ′ ′ EE 68 656 1 1 Ure LL6 – S3 – W1 30 – 24 – Granulitic See separate E 1165 1 L3 S2 W4 1–26 1–19 – 1160 Sn3 ′ ′ ′ ′ 1°53.08 6°46 12°53.839 4°40.00 16°24.50 0°49.944 12°56.788 16°13.87 16°03.98 16°14.94 16°40.89 11°47 3°56.14 3°46 4°31 4°25.75 4°23.16 4°38.90 3°53.22 3°56.66 3°45.83 3°56.10 3°58.61 ~8°09 11°54 3°52.19 4°18 7°20.535 10°12.336 11°41 Longitude (E or W) ′ ′ ′ ′ ′ 4°27.92 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′′ ′ ′′ ′ 16 36 ′ ′ ′ ′ ′ ′ ′ Latitude (N) Date found (mm/dd/yyyy) Place of recovery Gourara Algeria 11/2002 29°45.53 Hammadah al Hamra (HaH) HaH 330 Libya 03/17/2003 28°28.108 Djebel Chaab 003El Atchane 013 TiferineErg Algeria 12/14/2003 Algeria 11/2002 25°05.210 AlgeriaHaH 331 03/02/2001 29°58.50 27°16 Libya 03/19/2003 29°49.115 DaG 1040 Libya 2001–2002 27°16.88 DaG 1039 Libya 1999 27°19.81 DaG 1028 Libya 10/2000 27°04.54 DaG 1027 Libya 10/1999 27°13.86 Dar al Gani (DaG) DaG 1026 Libya 10/1999 26°54.42 Daraj 141 Libya 1987 29°35 Acfer 365 Algeria 11/2002 27°36.56 Acfer 360Acfer 364Acfer 367 Algeria 11/15/2002 Algeria 2002 27°29 Algeria 11/2002 27°42 27°41.06 Acfer 368 Algeria 11/2002 27°41.33 Acfer 369 Algeria 11/2002 27°40.02 Acfer 371 Algeria 11/2002 27°40.69 Acfer 372 Algeria 11/2002 26°36.70 Acfer 373 Algeria 11/2002 26°37.55 Acfer 375 Algeria 11/2002 27°30.51 Acfer 376 Algeria 11/2002 27°38.37 Acfer 377 Algeria 11/2002 27°39.75 Arlit Niger 02/2002 18°40.380 Benguerir Morocco 11/22/2004 ~32°15 Capot Rey Niger 03/2004 20°07.556 Daraj 131 Libya 03/20/1987 29°18 Name Acfer 324 Algeria 10/2001 27°30.05 Acfer 347 Algeria 2002 27°41 Daraj 114 Libya 01/19/1987 29°37 Table 1. Meteorites from Africa (named). Table Meteoritical Bulletin No. 89 A229 Silesia1 15.2 UPMCPa3 28.6 Mün5 20 Mün4 20 Mün4 47 NHMV2 20 Pa17 100, Type spec (g) Info § 57.6 a ringwoodite subtype 3.4 cv 004 entry entry fall; see sep- arate entry entry Fs (mol%) Comments Fa (mol%) Mass (g) Pieces Class Shock WG E 710 6 L6 S3 W1 25 21.5 – 24.9 Mün5 E 631 1 H5/6 S3 W2 19.5 17 terrestrial sv, E 662 1 H5 S2 W2 19 17 – 76.4 Mün5 E 111 1 H3 S2 W1 17.5 ± 2 14 ± 5 – 23 Mün6 E 880 24 H4/5 S2 W2–3 17 15.5 terrestrial cv 26 Mün6 ′ ′ ′ ′ ′ ed 4737 1 LL3 W1 27.5 ± 06 20.1 ± 6.8 – 26.5 UBP1 W 616 2 L6 S4 W0 25 21.1 – 616 Prato1 E 1800 1 H5 W3 19.7 18.1 Dakhla oasis 300 NHMV1 ′ ′ E 420 1 L6 S3 W1 25.3 21.5 – 420 Prato1 E 62285 66 H6 S2 W1 20.8 17.7 – 5022 Prato1 E 130 1 L6 S3 W4 24.9 21.1 – 120 Prato1 E 496 1 H5 S1 W4 18.2 16.4 – 496 Prato1 E 4334 53 L6 S3 W3 25.7 21.8 – 4334 Prato1 E 10000 3 L5 S4 W4 24.7 21.2 – 2906 Prato1 E 3000 1 L6 S4 W4 24.4 20.7 – 3000 Prato1 ′ ′ ′ ′ ′ ′ ′ E 4629W 2 17000 H5/6 Many S3 H3–5 W0 S4 20.3 W0 – 18 – Observed See separate ′ ′ isclosed 79.47 1 CO3 S1 W1–2 0–54 2 Possible ndisclosed 741 2 CV3 W3 0–25 1–15 – 21.1 UPMCPa3 2.9766°E 585 1 Lunar – – – – See separate 2.9766°E 13500 1 Lunar – – – – See separate 0°06.18 0°07.34 0°28.41 01°21.15 Longitude (E or W) 12°56.788 13°02.428 13°07.810 12°37.930 12°41.475 9°23 13°6 28°27.13 0°39.99 0°40.00 0°30.00 0°13.00 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ Latitude (N) ––– –– –– –– 150 –– 141 – 1 827 – 1 H4/5 – 87 1 S2 H5 220 1 H5/6 W2–3 S2 157 19 1 S1 H5 W3–4 72 1 20.5 H5 W4 S3 17 1 19 H5 S3 17.5 W3–4 19 H4 S2 W3–4 19 – 17 W3–4 S2 sv 18 17 W3–4 17 17 – 22 16.5 20 sv Mün3 Mün3 15 Prob. paired – 26 Mün3 19 – Mün3 20 Mün3 15 Mün3 Continued. Date found (mm/dd/yyyy) Kuke, Botswana Kuke, Botswana Kuke, Botswana Kuke, Botswana Kuke, Botswana Kuke, Botswana Kuke, Botswana 01/08/2004 12°50 10/16/2003 24°18 Place of recovery Niger Sahara Name HaH 332 Libya 03/19/2003 29°49.115 Sahara 99477Sahara 02502 Sahara 1999 Sahara 01/2002 Undisclosed Undisclosed Undisclosed Und 9220 7 L5 S6 W2 24.1 21.6 Veined, Sahara 02503Sahara 03502Sahara 03503 072Tanezrouft Sahara Sahara 05/2002 Sahara Algeria 01/2003 02/2003 11/2002 Undisclosed U Undisclosed Undisclos Undisclosed 24°26.29 Undisclosed 754 1 LL6 S2 W1 31.6 26.1 – 26.1 Pa20 Tanezrouft 073Tanezrouft Algeria 11/2002 24°25.44 Tanezrouft 074Tanezrouft Algeria 11/2002 24°13.33 Tanezrouft 075Tanezrouft Algeria 11/2002 24°04.10 HaH 333 Libya 03/19/2003 29°54.842 HaH 334 Libya 03/19/2003 30°02.073 HaH 335 Libya 05/29/2004 28°49.896 HaH 336 Libya 05/30/2004 28°39.041 Kalahari 002Kalahari 003Kalahari 004 Botswana in Purchased Kalahari 005 Botswana in Purchased Botswana in Purchased Kalahari 007 Botswana in Purchased Kalahari 008 Botswana in Purchased Botswana 09/1999 20.9818°S 2 Kalahari 001 Botswana in Purchased Kalahari 006 Botswana in Purchased Kalahari 009 Botswana 09/1999 20.9818°S 2 MabeMaigatari-Danduma Nigeria- Botswana 04/1999 21.3000° S E 24.1028° 378 1 H5 S2 W4 19 17 – 31 Mün3 Oum Dreyga West MatsitamaMut 002Plateau du Tademait Algeria Botswana 11/1999 11/2002 Egypt 21.0909°S 28°17.86 10/23/2003 26.4859°E 25°35.99 187 1 H4/5 S3 W2 19 17 – 20 Mün3 Plateau du Tademait 003Plateau du Tademait Algeria 11/2002 28°17.90 Plateau du Tademait 004Plateau du Tademait Algeria 11/2002 28°18.00 Plateau du Tademait 005Plateau du Tademait Algeria 11/2002 27°53.50 Table 1. Meteorites from Africa (named). Table A230 S. S. Russell et al. 20 Mün2 23.5 Pa16 30.2 Pa16 28.5 Pa16 34.8 Pa16 35.1 Pa16 22.2 Pa21 23.5 Pa16 Type spec (g) Info § a a few meters from Zillah 001 very friable entry (1 mm) crust parallel black veins subtype 3.7 entry entry V; 61 g, MNB; (4) breccia, shock grade V; Fs (mol%) Comments Fa (mol%) ditional material: 87.1 g, NHM additional 67.94 g at NHM; (3) ad Mass (g) Pieces Class Shock WG E 172 1 Euc S3 W1 – 61 ± 1.2found cv; sv; E 1149 1 CO3 – – – – See separate E 1475 1 L6 S3 W1–2 24.5 20.5 – 20 Mün2 ′ ′ ′ WW 3548W 217 1599 5 1 1 L6 L4 L6 S4 S2 S3 W2 W2 ± 0.4 25.6 W2 21.4 ± 0.34 25.3 ± 0.4 25.8 ± 0.6 – 21.6 ± 1.1 21.6 ± 0.5 4 – 27.2 Pa16 20.5 24.6 Pa16 Pa16 W 1056 1 L(LL)5 S2 W2 ± 0.4 26.2 22.1 ± 0.9 – 24.9 Pa16 EE 136 320 1 1 H5 H5 S2 S2 W2 W3 ± 0.2 19.6 ± 0.2 20.6 17.6 ± 0.9 18.0 ± 0.3separate See 30.7 Pa16 W 1012WW 265 1 369 1 CM2E 1 L(LL)6 90.4 S2 L6 1 W2/3 W3 0.4–64.4 S4 H3 ± 1.6 26.6 0.9–14.9 23.0 ± 2.4 W2 S5 See separate fusion Thick 25.6 ± 0.5 W2 21.5 ± 0.8of 0.84–37.5 Networks 4.1–21.2 Estimated W 1031 1 H6 S1 W2/3 19.6 ± 0.2 17.4 ± 0.2 – 33.3 Pa16 E 213 1 H5 S1 W1 18.8 ± 0.3 16.6 ± 0.2porous, Very ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ W 2650 1 L6 S2 W2 24.7 20.9 – 2650 Prato1 W 5150 1 H5 S2 W3 19.3 16.9 – 5150 Prato1 E 1058 1 L5 S2 W2 24.6 21.1 – 1050 Prato1 ′ ′ ′ 17°01.110 0°33.702 0°32.377 0°31.448 0°31.118 Longitude (E or W) 0°34.157 0°11.909 0°03.373 0°16.075 0°26.056 0°30.862 0°26.075 0°02.339 11°51.000 0°31.00 0°31.00 4°38.00 17°01.110 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ paired with Acfer 270; (2) an ′ ′ ′ Latitude (N) Continued. Date found (mm/dd/yyyy) O = +1.438, +1.396‰; likely to be 18 δ Place of recovery 1.619‰; − 1.568, − O = 17 δ variable up to S4 between clasts. Abbreviations: sv = shock veins; cv calcite veins. Tanezrouft 077Tanezrouft 078Tanezrouft 079Tanezrouft Algeria Algeria 12/21/2003 Algeria 12/21/2003 12/22/2003 24°37.267 24°44.144 24°34.815 Name 076Tanezrouft Algeria 12/20/2003 24°37.230 Tanezrouft 080Tanezrouft 081Tanezrouft Algeria Algeria 12/22/2003 12/18/2003 24°39.264 25°14.419 Tanezrouft 086Tanezrouft 087Tanezrouft Algeria Algeria 12/23/2003 12/23/2003 25°17.423 25°45.366 Tanezrouft 082Tanezrouft 083Tanezrouft 084Tanezrouft Algeria 12/20/2003 Algeria 085Tanezrouft 12/22/2003 Algeria 24°49.036 12/22/2003 24°38.883 Algeria 008Tiffa 24°45.366 12/23/2003 25°12.770 Niger 10/2001 20°21.500 Touat 001Touat Algeria 11/2002 27°38.12 Touat 002Touat Algeria 11/2002 27°28.00 Zelfana Algeria 11/2002 32°09.50 Zillah 001 Libya 12/10/1990 29°02.220 Zillah 002 Libya 12/10/1990 29°02.220 (1) Table 1. Meteorites from Africa (named). Table a Meteoritical Bulletin No. 89 A231 La12 Info La4 La6 La5 a CyDL 222? CyDL 063? CyDL 040? CyDL 223? Type (g) Comment Wo (mol%) Fs (mol%) Fa (mol%) 1.47 1 L6 S3 W1 23.8 – – 0.65 Paired to 4.4 1 H6 S2 W4 18.3 – – 4.4 – La4 3.2 1 H56.1 S2 1 W5 H4 S2 18.7 W3 – 199.87 – 1 – H5 3.2 – S2 – W3 5.9 La4 – 16.1 La4 – 2.15 – La12 4342.5736.35 1 1 1 H5 L6 H6 S2 S3 S1 W3 W4 W3 18.3 24.4 18.1 – – – – – – 10.21 9.1 – 9.09 – – La12 La12 La12 67.61 1 H4 S261.568.02 4 W1 3 H5 18.5 H4 S218.5 S314.2 – 1 W4 W3 1 H517.4 18.9 – 19.2 H4 S1 118.3 S210.4 – 1 – W4 H432.22 15.1 1 W290.04 1 Paired to S2 H510.84 18.8 – 1 – H413.87 18.7 1 H4 S2 W317.02 1 H6 S217.7 – S2 1 H5 W576.88 – 18.6 15.8 S2 H5 1 W4 13.5 S2 1 W3 – H416.66 – 18.5 S2 – W5 H5 – 19.1 S2 – 1 W4 H5 18.9 W3 S2 19.3 – S2 W2 H5 La7 19 – 17.95 La7 – – W4 18.8 – S3 W1 2.8 – 18.6 – – 18.6 – – W5 – 17.9 – 17.2 – – La7 – 18.3 – 17.1 – – – La7 – 3.1 10.2 – – 22.92 – – – La7 2 – 2.79 3.99 La8 2 – – 5.07 La7 – La4 5.8 15.44 La12 – – La12 3.7 La12 La12 – La12 La4 La12 187.55 2 H6 S3 W1 18.4 – – 19.58 – La12 798 1 H3–5 S2 W1 16.1 13.3 – 34.7 – Ca1 338106.7255.72 1 2 1 H5 H5–6344 H5 S2 S2 S2 1 W3–W6 W3 19.6 W3 H4 18.6 S2 16.1412.05 18.7 2 W2278.1 – – – 4 L6 18.8 – S3 H5 – 22.1162 – W5 S2 2 1 22.7 W3 25.4 36.73 – –140 – H3 La4 18.6 – S2 1117.5 20.5 La4 – W3 La5 H5 1 Paired to – S2 18 H5 – W3 S2 25.5 – Paired to W3 18.6 20.5 – 19.2 – – – La5 – 33.2 – – 20.6 – La4 22.5 – La4 La8 3650 2 L6 S4 W2 24.5 – – 26.4 1 La3 24305220 2 6 392.8 H52134 H5 1 S2 14 S21364.31 H5 W3 6 H5 W4 S2 S2 18.8 H5 W3 18.7 W4 S21369 – 18.7 – W5 18.7 21 – – 18.4 H5–6 – – S2 – – W3–W4 20.23 – 19 – 27.9 – – 35.5 – 24.9 – La5 – La6 25.2 – – La4 La6 27.4 La6 2 La5 Mass (g) Pieces Class Shock WG ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ Longitude (W) 46.442 45.718 45.259 43.803 45.170 114º11.500 114º12.53 46.140 46.01 43.855 45.239 46.323 46.578 45.806 44.800 46.002 46.380 46.458 45.186 45.670 46.019 44.128 46.123 44.666 45.186 46.123 46.110 45.012 44.964 44.908 45.650 45.987 45.923 44.912 43.421 43.419 45.823 46.143 46.123 45.777 46.066 46.200 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ Latitutde (N) 35º + + 116º Date found (mm/dd/yyyy) from North and South America. Mohave, AZ 01/15/2002 35º52.050 Mohave, AZ 01/28/2004 34º43.472 fan Pediment terrace North America (USA) Bluebird Alluvial CyDL 165CyDL 175CyDL 176 Dry lakeCyDL 194 Dry lakeCABernardino, San 02/18/2002 Dry lakeCABernardino, San 12/13/2002 Dry lakeCABernardino, San 4.133 01/02/2003CABernardino, San 3.285 09/01/2004 3.271 5.303 Name Find site State County, CyDL 116 Dry lakeCABernardino, San 07/22/1999 3.508 Buck Mountain Wash Coyote Dry Lake (CyDL) CyDL 001 Dry lakeCABernardino, San 05/25/1995 3.01 CyDL 117 Dry lakeCABernardino, San 07/23/1999 3.006 CyDL 002CyDL 003CyDL 024 Dry lakeCyDL 033 Dry lakeCABernardino, San CyDL 040 12/13/1998 Dry lakeCABernardino, San 12/21/1998 Dry lakeCABernardino, San 2.852 CyDL 054 06/01/1999 Dry lakeCABernardino, San 5.285 CyDL 061 01/13/1999CABernardino, San 4.290 CyDL 063 Dry lake 01/16/1999 3.363 Dry lakeCABernardino, San CyDL 064 5.624 01/16/1999 Dry lakeCABernardino, San CyDL 067 01/20/1999CABernardino, San 4.600 Dry lake 01/21/1999CyDL 080 3.145 Dry lakeCABernardino, San CyDL 105 3.527 01/21/1999CABernardino, San CyDL 110 Dry lake 01/21/1999 3.490 CyDL 115 Dry lakeCABernardino, San 2.289 01/31/1999 Dry lakeCABernardino, San 04/17/1999 Dry lakeCABernardino, San 4.441 CyDL 119 04/17/1999CABernardino, San 3.044 CyDL 120 04/07/1999 2.775 CyDL 121 Dry lake 3.519 CyDL 129 Dry lakeCABernardino, San CyDL 130 07/24/1999 Dry lakeCABernardino, San CyDL 132 07/08/1999 Dry lakeCABernardino, San 2.289 CyDL 134 07/08/1999 Dry lakeCABernardino, San 3.536 CyDL 138 11/02/2000 Dry lakeCABernardino, San 3.568 CyDL 139 11/02/2000 Dry lakeCABernardino, San 4.150 CyDL 142 02/19/2000 Dry lakeCABernardino, San 4.071 CyDL 151 08/04/2000 Dry lakeCABernardino, San 4.217 CyDL 152 08/04/2000 Dry lakeCABernardino, San 5.550 CyDL 153 08/04/2000 Dry lakeCABernardino, San 3.170 CyDL 155 05/05/2000 Dry lakeCABernardino, San 3.170 CyDL 159 02/16/2001 Dry lakeCABernardino, San 4.035 CyDL 160 02/16/2001 Dry lakeCABernardino, San 3.361 CyDL 162 07/03/2001 Dry lakeCABernardino, San 3.364 CyDL 163 04/15/2001 Dry lakeCABernardino, San 4.417 CyDL 164 11/16/2001 Dry lakeCABernardino, San 4.108 01/13/2002 Dry lakeCABernardino, San 3.519 01/13/2002 Dry lakeCABernardino, San 3.691 08/02/2002CABernardino, San 4.681 08/02/2002 4.200 3.501 Table 2. Ordinary Chondrite finds Table A232 S. S. Russell et al. Info La5 La7 La7 a LV 041? LV CyDL 194? CyDL 067? Type (g) Comment Wo (mol%) Fs (mol%) Fa (mol%) 5.63.1 1 1 L5 L6 S1 S2 W5 W5 24.3 24.2 – – – – 1.05 – 1.02 – La12 La12 5.21 10.842.17 1 L61.75 1 1 L6 S3 L6 S3 L4 W5 S52.29 S3 W29.2 25.0 ± 0.5 1 W4 – W3 1 24.5 ± 0.4 H4 24.2 ± 0.4 – 23.9 ± 0.6 L6 – S3 – – S2 – W3 – W5 – 1.5 18.8 ± 0.3 – Paired to 23.7 0.22 – 0.78 – 0.4 20.4 –6.55 – 1 1.4 La5 La14 L5/6 0.79 La5 – S3 1.9 – W3 La5 25.7 La12 21.8 0.47 1.3 – Ha4 54.31 1 H4 18.145 16.7 1 1.2 H4 S2 12.1 W3 –21 19.3 1 NAU7 H4 17.4 S2 – W538.5610.32 1 17.830.43 1 9.2 1 L6 – L6 –32.5 S2 L6 S3 1 S2 W3 – USA7 W4 L5 W5 24.0 ± 0.5 24.4 ± 0.3 – 24.5 ± 0.4 – 5 – W4 – – – 24.5 –17.9 1 La13 8.62 20.9 – 2.7 7.99 L5 – 1.3 – S3 La6 W2 La6 6.7 La6 – 24.6 20.9 Ha5 1.07 6 – Ha4 22.5 116.36 L581.4 171.8 S2 1 H6 1 W1 LL6 S3 H4 S4 23.7 W3 S2 W2 – W2 19.1 28.1 18.1 16.4 – – 15.9 1.1 – 4.85 – Paired to 3.64 – 16.4 14.22 – – La12 La4 La9 490301 1 1 H4 S3 H4 S1 W2 W3 18.4 18.4 16.1106.22 – 1.1 1 L6 – 20.6 S3 – W3370 26 3 25.6 ± 0.4 Asu5 1 – L5860 La2 S2 – 1 W2 H5 23.04 24.8 – S1 20.8 W2 La12 – 19.2 16.7 30 1.6 – 680 UAriz1 4 Asu7 512 8 L6 S4 W5 24.9 – – 30.6 Paired to 41003700 1 1 H3.8 S1 L5 W3 S3 17.7 ± 4.2 W1 16.5 ± 0.4 1.3 ± 0.3 4100 24.6 – 20.3 1.9 Asu4 192.3 – Asu2 242013063400 1 1 1 H49158 H4 S2 LL4 2 S2 S1 W5 L6 W3 W2 18.3 S4 18.8 28.8 W2 – – 23.1 25 – – – 21 35.1 412 25.2 1.39 – – – 129 La10 – Asu3 La11 Ca3 8600 1 H5 S3 W1 17.6 15.9 1.1 8500 – TCU1 Mass (g) Pieces Class Shock WG 29500 1 H5 S1 W1 19.2 17.1 – 20.2 – Asu6 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ Continued. ′ ′ ′ ′′ ′ ′ ′′ ′ ′ ′ ′ ′ ′ ′ ′ ′ 34 ′ Longitude (W) 116º57.202 43.230 102º59.4 112º37 112º56.52 105º48 96º15 105º42 116º56.127 116º56.530 116º56.585 6.566 116º 116º57.822 116º57.753 116º57.650 116º57.907 116º58.410 116º58.434 116º57.5 116º57.664 115º59.802 118º24.62 118º25.002 118º24.551 103º50.42 102º22.5 114º11.485 114º01.920 114º02.603 45.332 45.491 45.004 44.026 44.762 99º24'21 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′′ ′ ′ ′′ ′ ′ ′ 32 23 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ Latitutde (N) Date found (mm/dd/yyyy) from North and South America. no, CA 11/10/2003 34º29.229 ng, NV 11/05/2003 40º37.699 Maricopa, AZ 01/07/2000Park, CO 33º2 Alamosa, CO 2000 1937 38º50 37º41 Pershing, NV Spring 1999 COWeld, 40º37.59 Mohave, AZ 1995 11/03/2004 34º42.874 40º37.55 McCulloch, TX 05/04/2003Kit Carson, CO 31º23 1972 or 1973 39º13.8 basin Dry wash Millard, UT rie Desk 04/27/2004Sandy 39º29.48 KS Riley, bank 05/05/2004 39º16 Dry lake Nye, NVroadway 08/16/2003lands 38º23.951 Pediment terrace field field LV 027LV 040LV 041LV Dry lake Dry lakeBernardi San San Bernardino CA Dry lake 03/16/2004CABernardino, San 03/16/2004 34º29.526 34º29.385 NameCyDL 221 Find site Dry lake State County, CABernardino, San 05/12/2003 3.430 CyDL 222 Dry lakeCABernardino, San 08/05/2004 2.405 BendGila Greener Desert Reservoir Hartsel Kansas State University Open prai- Little Spring Creek (LV) Lucerne Valley 025LV LV 026 Dry lake Dry lakeCABernardino, San 04/08/2003 San Bernardino, CA 042LV 09/27/2003 34º30.652 043LV 044LV 34º30.006 045LV Dry lake 046LV Dry lakeCABernardino, San 047 03/26/2004LV Dry lakeCABernardino, San 048 03/26/2004LV Dry lakeCABernardino, San 34º29.157 049 04/23/2004LV Dry lakeCABernardino, San 34º29.074 09/07/2004Lunar Dry Dry lakeCABernardino, San 34º29.048 Lake 09/07/2004 Dry lakeCABernardino, San 34º29.220 Majuba 09/07/2004 Dry lakeCABernardino, San 34º29.245 09/07/2004CABernardino, San Majuba 002 34º29.168 12/11/2004Majuba 003 34º29.2 Desert PlacersNew Raymer 34º29.083 Placersgrass Open Pershi Ovid (b) Pershing, NV Palo Verde Mine Sandy soilRed Dry Lake (RdDL) 10/10/2003 Sedgwick, CORdDL 024 40º37.847 RdDL 025 1943 Dry lake Dry lake Mohave, AZ Mohave, AZ 40º45.5 09/13/2003 09/28/2003 35º41.839 35º40.768 CyDL 223CyDL 230 Dry lakeCyDL 235CABernardino, San CyDL 249 Dry lake 08/05/2004Fife Dry lakeCABernardino, San 2.305 06/13/2004 Dry lakeCABernardino, San Flagler 10/07/2004CABernardino, San 5.375 10/24/2004 3.377 Wheat 5.255 Ploughed Table 2. Ordinary Chondrite finds Table Meteoritical Bulletin No. 89 A233 Sn1 Pd1 Info Info a a Type (g) Comment entry entry meteorite in E. King collection; (4) Wo (mol%) Mag. Sus Comment Fs (mol%) Fs (mol%) Fa (mol%) Fa (mol%) paperweight. Listed as unclassified Kansas present; (3) used as a 5.25 1 H4 S2 W3 18.2 – – 1.6 – La4 11.3 159.2 H4 1 S2 H6 W238.9 S2 1 18.3 W3 H5 – 18.6 S2 W2 – – 18.6 – 4 – – 16.02 – 5 La4 8.02 La12 – La9 307.75 1 L6 S2 W3 25 – – 26.63 – La12 5000 1 H5 S1 W1 19.7 17 1.3 5000 – Asu8 Mass (g) Pieces Class Shock WG ~2000 1 LL6 S2 W2 33 27 – 70 – SAm1 ′ ′ ′ ′ ′ Continued. ′ by Huss; (5) possibly a fragment of Primm. ′ ith shock stage up to S4 Longitude (W) 114º02.071 114º02.624 115º22.030 103º41.83 117º01.577 117º0.971 9.02 1 H6 S3 W1 20.9 17.4 5 br Rm1 3.99 1 H6 S2 W1 19.5 17.2 4.98 – Rm1 4.67 1 H6 S22.71 1 W1 19.4 H5 17.1 S2 4.99 W1 br; veined 19.6 18 Rm1 5.04 – Rm1 4.84 1 Acap-Lod – –2.65 – 1 H5 – S2 – W1 Gabbro; see separate 19.4 17.8 5.23 – Rm1 3.26 1 H5 S2 W2 19.8 17.5 4.65 – Rm1 8.4 1 H3 S2 W2 181.41 1 17 H~5 – – – br – – Sn1 5.47 – Sn1 3.19 1 Ure – – – – – pbr; see separate entry Sn1 0.93 1 Euc – Low 328.64 1 36 LL3 – S2 br W1 4.2–23.8 10.1–33.1 3.98 – Sn1 Rm1 7.13 1 H6 S2 W1 19.4 16.8 5.01 – Rm1 17.39 1 H5 S2 W1/2 19.5 17.5 5.12 – Rm1 20.66 1 EL4 – – – – 5.15 See separate entry Sn1 31.89 123.94 1 Ure L6 – S5 – W1 – 25 – 21 – – see separate mbr; Veined Sn1 10.5 1 H5 S1 W1 19.5 17.5 5.11 – Rm1 12.45 1 H4–6 S3 W2 1810.1 1 16 L6 – S5 br W1 25.2 21.3 Sn1 4.64 – Rm1 13.55 1 H3 S2 W1 17 (11–20) 14 (10–17) – br Sn1 ′ ′ ′ ′ ′ ′ Mass (g) Pieces Class Shock WG S 70º19.2 ′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ Latitutde (N) 12.6 35.4 11.9 38.8 18.6 29 03.3 14.9 18 29 50.3 18 50.5 16 51.4 27 51.4 30 47.0 04 47.0 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ 160°28 160°28 160°30 160°29 160°30 160°31 160°29 160°23 160°31 160°26 160°26 160°30 160°26 160°30 160°32 160°30 160°32 160°30 160°24 160°30 Longitude (W) 160°29 Date found (mm/dd/yyyy) 10/01/2001 25º8.6 ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ from North and South America. 09.7 11.1 04.7 09.8 04.0 08.4 20 18.5 07.8 22 22 05.3 20 06.7 20 06.1 27 06.1 27 04.7 44 ich is an H6: detailed comparison provided ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ Latitude (S) Basin (L4, W3); (2) genomict breccia, clasts w II Region, Antofagasta Date found (mm/dd/yyyy) desert FRO 03019 12/29/2003 72°57 FRO 03018 12/29/2003 72°57 FRO 03009 12/28/2003 72°57 FRO 03017 12/29/2003 72°57 FRO 03008 12/28/2003 72°57 FRO 03016 12/28/2003 72°57 FRO 93001 04/01/1994FRO 03005 01/01/2004 72°57 72°57 FRO 03015 12/28/2003 72°57 FRO 90233 10/01/1991FRO 90235 10/01/1991 72°57 72°57 FRO 03014 12/28/2003 72°57 FRO 90225 10/01/1991 72°57 FRO 03013 12/28/2003 72°57 FRO 90200 10/01/1991 72°57 FRO 03012 12/28/2003 72°57 FRO 90198 10/01/1991 72°59 FRO 03011 12/28/2003 72°57 FRO 90182 10/01/1991 72°59 FRO 03010 12/28/2003 72°57 Name Frontier Mountain (FRO) Frontier FRO 90127 10/01/1991 72°57 does not appear to be paired with Ovid, wh NameRdDL 028 Find site Dry lake State County, Mohave, AZ 04/24/2004 35º38.688 RdDL 029Roach Dry Lake (RhDL) Dry lakeRhDL 021Stoneham Mohave, AZ Dry lake (SuV) Superior Valley land Farm NVSuV 020 Clark County, 04/24/2004 CO Weld, SuV 022 12/29/2001 35º37.609 South America (Chile) Dry lake 35º40.379 synonym for Viedma Balneario el Condor, Dry lakeCABernardino, San 1960sPaposo 05/01/2003CABernardino, San 10/25/2004 35º14.315 35º14.223 Rocky 40º38.27 (1) Clearly not paired with Gold Table 3. Meteorites from Frontier Mountain, Antarctica. Table Table 2. Ordinary Chondrite finds Table a A234 S. S. Russell et al. Info a Mag. Sus Comment Fs (mol%) Fa (mol%) 3.44 1 H6 S5 W1 18.6 17.2 5.02 – Pd1 4.51 1 H6 S2 W1 18.6 17.1 5.02 – Pd1 3.35 1 H5 S2 W1 18.95.54 1 17.5 H6 5.12 S2 br W1 18.5 17.2 Pd1 4.97 – Pd1 9.57 1 H5 S2 W2 17.9 16.5 4.94 – Sn1 1.31 1 H5 S2 W1 19.1 17.3 5.27 – Pd1 1.63 1 H3 S1 W2 18.1 2–17 4.88 – Sn1 5 1 L3–6 S4 W03.15 12.0–27.5 1 2.9–26 4.64 L3 br S2 W18.18 0.45–30.6 1 1.2–22.5 Pd1 4.14 L3 – S4 W0 8.6–25.7 Pd1 2–26 4.19 – Pd1 1.75 1 H3–4 S1 W2 3–38 4–20 4.6 Dark inclusions Sn1 7.76 1 L6 S3 W1 22.44.47 1 17.8 L4 5.14 S2 br W0 26.19.75 1 20.1 Pd1 H6 4.44 S2 Veined W1 18.5 Pd1 17 4.96 – Pd1 1.59 1 H6 S1 W1/2 19.6 16.7 4.97 Veined Sn1 3 1 H6 S2 W17.18 19 1 H5 17.4 S2 5.08 – W1 19.48.23 1 18 H4/5 Pd1 S2 4.92 br W1 19.5 17.6 Pd1 5.17 – Pd1 2.42 1 H6 S1 W2 18.2 16.4 4.87 – Sn1 1.53 1 H4 S2 W3 18.49.96 1 16.8 L5 4.86 S4 – W1 24.1 20.9 Pd1 4.62 br Pd1 1.84 1 H6 S2 W1 19.46.74 1 17.5 H5 5.04 S2 – W1 19.33.71 1 17.6 H6 Pd1 5.02 S2 – W1 18.4 16.9 Pd1 5.11 – Pd1 3.84 1 H5 S2 W1 17.7 16.2 5.1 – Sn1 2.47 1 Ure – –2.55 1 H~5 – – 3.985.4 pbr; see separate entry – Pd1 1 H6 – S3 5.16 W2 – 19.3 18 Sn1 4.85 – Pd1 3.37 1 H4 S2 W2 17.8 16.4 4.93 – Sn1 1.36 1 L6 S4 W0/1 25.32.97 1 21.5 L6 4.82 – S4 W0 256.32 1 Rm1 22 H4–5 S2 4.68 W1 – 18.1 16.9 5.14 Pd1 – Pd1 0.94 1 L6 S4 W0/4 24.1 21.9 4.61 – Sn1 15.47 1 H4 S3 W2 1521.54 1 14.5 H6 4.83 S2 – W1 18.8 17.2 Pd1 4.94 – Pd1 28.1 1 L4 S1 W112.31 26 1 H3–4 22.1 S2 4.35 W2 – 18.1 16.5 Pd1 4.8 br Pd1 26.11 1 H5 S2 W1 18.6 17 5.06 br Pd1 10.17 1 H5 S2 W1 18.6 17.2 5.13 br11.77 2 Pd1 L3 S4 W0 0.6–25.5 3.6–25.7 4.43 – Pd1 11.55 1 H5–6 S2 W1 18.9 17.4 4.87 – Pd1 61 1 L6 S5 W1/2 24.2 20.6 4.71 – Sn1 Continued. Mass (g) Pieces Class Shock WG ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ 33.8 57.9 51.5 54.8 51.3 31.7 54.0 50.7 31.7 50.4 54.0 50.7 59.0 18.2 53.5 49.4 59.0 21.8 03.5 47.7 02.1 25.3 43.7 47.7 22.0 54.3 06.0 46.9 21.0 26.1 16.5 43.0 20.0 29.7 35.8 33.8 20.0 32.6 12.6 33.8 11.4 41.8 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ 160°27 160°30 160°30 160°27 160°29 160°30 160°29 160°29 160°30 160°29 160°23 160°29 160°30 160°27 160°24 160°29 160°30 160°27 160°24 160°27 160°30 160°28 160°26 160°26 160°30 160°29 160°26 160°27 160°30 160°31 160°27 160°27 160°30 160°31 160°27 160°27 160°30 160°31 160°27 Longitude (W) 160°28 160°30 160°31 ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ 06.9 08.8 07.3 04.9 10.1 09.9 03.9 12.9 09.9 05.8 12.9 43.5 09.9 05.8 08.0 20.3 09.9 05.8 08.0 16.8 15.2 05.2 09.3 11.1 09.4 05.2 12.0 08.7 09.6 05.4 07.8 09.9 06.3 05.6 07.0 05.9 03.2 07.3 07.0 04.7 09.7 07.3 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ Latitude (S) Date found (mm/dd/yyyy) FRO 03032 12/28/2003 72°57 FRO 03043 12/28/2003 72°57 FRO 03054 12/29/2003 72°57 FRO 03031 12/28/2003 72°57 FRO 03042 12/28/2003 72°57 FRO 03053 12/29/2003 72°57 FRO 03030 12/28/2003 72°57 FRO 03041 12/28/2003 72°57 FRO 03052 12/29/2003 72°57 FRO 03029 12/28/2003 72°57 FRO 03040 12/28/2003 72°57 FRO 03051 12/29/2003 72°57 FRO 03063 03/01/2004 72°59 FRO 03028 12/28/2003 72°57 FRO 03039 12/28/2003 72°57 FRO 03050 12/29/2003 72°57 FRO 03062 03/01/2004 72°59 FRO 03027 12/28/2003 72°57 FRO 03038 12/28/2003 72°57 FRO 03049 12/29/2003 72°57 FRO 03061 03/01/2004 72°59 FRO 03026 12/29/2003 72°57 FRO 03037 12/28/2003 72°57 FRO 03048 12/29/2003 72°57 FRO 03060 12/29/2003 72°57 FRO 03025 12/29/2003 72°57 FRO 03036 12/28/2003 72°57 FRO 03047 12/29/2003 72°57 FRO 03058 12/29/2003 72°57 FRO 03024 12/29/2003 72°57 FRO 03035 12/28/2003 72°57 FRO 03046 12/28/2003 72°57 FRO 03057 12/29/2003 72°57 FRO 03023 12/29/2003 72°57 FRO 03034 12/28/2003 72°57 FRO 03045 12/28/2003 72°57 FRO 03056 12/29/2003 72°57 FRO 03022 12/29/2003 72°57 FRO 03033 12/28/2003 72°57 FRO 03044 12/28/2003 72°57 FRO 03055 12/29/2003 72°57 Name FRO 03020 12/29/2003 72°57 Table 3. Meteorites from Frontier Mountain, Antarctica. Table Meteoritical Bulletin No. 89 A235 Info a Mag. Sus Comment Fs (mol%) Fa (mol%) 0.74 1 H4 S2 W2 17.8 16.4 4.91 – Sn1 0.41 1 H6 S1 W0 20.1 17.8 5.08 –0.41 1 H~5 Sn1 – – – – 5.2 – Sn1 1.94 1 H4 S3 W0 18.12.51 1 16.7 H3–5 5.2 S2 – W1 24-300.78 1 8–22 L6 Sn1 5.13 – S1 W1 23.8 Sn1 20.8 4.51 – Sn1 0.17 1 H5/6 S3 W2 18.48.25 1 17 H3–6 4.9 S2 Veined W2 1–180.21 1 9–19 Sn1 H~5 4.79 – – – – Sn1 – 5.25 – Sn1 0.46 1 H3 S1 W13.16 7–22 1 5–22 H4–6 4.88 S2 – W1 18.20.85 1 16 Sn1 L6 4.93 – S3 W1 23.3 21 Sn1 5.01 – Sn1 1.52 1 H3–6 S2 W2 18.1 16.5 4.81 –2.29 1 Sn1 H6 S4 W1 17.8 17.5 5.05 – Sn1 0.73 1 H3 S1 W1 14–172.05 1 6–15 H3 4.94 – S2 W2 14–260.7 1 5–17 Sn1 H3 4.83 – S1 W2 1–26 Sn1 10–18 4.46 – Sn1 2.25 1 H3 S1 W1 17.1 13–20 4.84 –6.1 1 Sn1 L6 S5 W1 24.6 20.4 4.53 – Sn1 4.34 1 H6 S2 W1/2 17.51.43 1 16.2 L6 4.74 br S4 W2 24.45.6 1 Sn1 21 H3/4 4.29 S1 – W1 19.9 17.6 Sn1 5.09 – Sn1 3.51 1 H4 S2 W1 17.5 16 4.95 –8.76 1 H4 Sn1 S4 W0 17.1 16.1 5.14 – Sn1 0.95 1 H4 S4 W1 17.7 15.9 5.33 – Sn1 12.05 1 H5 S2 W1 17.914.96 1 16.6 H5 5.3 S1 – W2 18.5 17.3 Sn1 5.05 – Sn1 19.51 1 H5 S1 W2 18.6 16.4 4.82 – Sn1 42.9 1 H4 S1 W1 18.4 17.4 4.8 – Sn1 19.1 1 H6 S3 W1 19 16.8 5 – Sn1 26.43 1 H5 S2 W1 17.6 16.2 4.98 –16.07 1 H4 Sn1 S4 W0 17.8 16 5.16 – Sn1 17.16 1 H5 S4 W1 17.9 16.5 4.95 – Sn1 24.27 1 H4 S3 W1 17.5 17.2 5.05 – Sn1 Continued. 352.2 1 H5 S4 W1 17.1 16.2 5.16 – Sn1 Mass (g) Pieces Class Shock WG ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ 16.1 27.7 05.8 32.3 44.2 35.9 33.2 37.4 35.9 35.3 37.4 55.1 59.7 38.2 51.7 55.5 21.7 44.4 21.3 26.2 14.9 25.0 29.9 20.4 38.4 37.1 29.4 41.7 38.9 23.7 03.8 50.4 11.1 49.5 03.8 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ – polymict breccia. 160°30 160°27 160°28 160°30 160°26 160°23 160°30 160°26 160°23 160°30 160°26 160°23 160°30 160°23 160°23 160°30 160°23 160°24 160°30 160°23 160°24 160°24 160°23 160°26 160°23 160°23 160°26 160°23 160°23 160°26 160°41 160°30 Longitude (W) 160°23 160°29 160°41 ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ 40.8 08.2 08.4 24.1 08.0 12.2 41.2 06.4 12.1 43.7 06.4 10.7 43.7 05.8 40.3 43.1 05.2 41.5 19.9 05.2 42.6 16.0 39.2 41.5 14.9 42.1 44.3 09.2 38.2 44.1 10.1 51.6 08.2 43.5 14.3 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ nomict breccia; pbr Latitude (S) Date found (mm/dd/yyyy) FRO 03076 12/29/2003 72°57 FRO 03087 01/01/2004 72°57 FRO 03098 03/01/2004 72°57 FRO 03074 04/01/2004 72°57 FRO 03086 12/31/2003 72°57 FRO 03097 03/01/2004 72°57 FRO 03073 04/01/2004 72°57 FRO 03085 12/31/2003 72°59 FRO 03096 03/01/2004 72°57 FRO 03072 04/01/2004 72°57 FRO 03084 12/31/2003 72°59 FRO 03095 03/01/2004 72°57 FRO 03071 04/01/2004 72°57 FRO 03083 12/31/2003 72°59 FRO 03094 03/01/2004 72°57 FRO 03070 03/01/2004 72°59 FRO 03082 12/31/2003 72°59 FRO 03093 03/01/2004 72°57 FRO 03069 03/01/2004 72°59 FRO 03081 12/31/2003 72°59 FRO 03092 03/01/2004 72°57 FRO 03068 03/01/2004 72°59 FRO 03080 12/31/2003 72°59 FRO 03091 02/01/2004 72°59 FRO 03067 03/01/2004 72°59 FRO 03079 12/29/2003 72°57 FRO 03090 02/01/2004 72°59 FRO 03066 03/01/2004 72°59 FRO 03078 12/29/2003 72°57 FRO 03089 02/01/2004 72°59 FRO 03065 03/01/2004 72°59 FRO 03077 12/29/2003 72°57 FRO 03088 01/01/2004 72°57 FRO 03099 03/01/2004 72°57 Name FRO 03064 03/01/2004 72°59 Abbreviations: br – brecciated; mbr mo Table 3. Meteorites from Frontier Mountain, Antarctica. Table a A236 S. S. Russell et al. –NU 15.6 ± 12.3 (7.8–29.8) Fs (mol%) Comments Info (8.9–23.5) Fa (mol%) 8.9 L5 S3 W1 24.3 20.4 – CAS 6.6 CO3 – – – – See separate entry CAS 5 L5 S4 W2 23.87 L4 20.8 S3 – W1 ± 0.7 24.3 20.6 ± 0.5 CAS – CAS 7.5 Martian – – – – separate entry See CAS 3.6 CM2 – – – – See separate entry CAS 8.7 H5 S1 W1–2 18.7 18.5 – NU 2.2 CM2 – – – – See separate entry CAS 7.4 LL4–6 S1 W1 28.3 ± 0.4 23.0 ± 2.9 – CAS 2.5 LL3 S1 W1 14.4–48.3 4.1–5.9 – NU 8.5 H5 S1 W2 18.6 15.5 –3.6 LL6 CAS S1 W1 31.6 26.2 – CAS 0.4 CM2 – – – – See separate entry NU 612 L6 S1 W1 24.2 20.9 – CAS 51.7 H5 S1 W2 18.4 16.2 – CAS 54.2 L5 S2 W1 24.5 20.5 – CAS 19.1 L6 S3 W2 2417.2 H380.6 H5 20.9 S1 S2 – W3 W2 16.9 ± 6.4 18.9 CAS 16.8 – CAS 23.5 Pallasite – – – – separate entry See CAS 39.6 L4 S1 W1 26.4 ± 0.7 21.7 ± 0.3 – CAS 18.6 L5 S3 W1 23.925.4 L6 20.4 S2 – W2 25.1 CAS 23.9 – NU 72.9 H5 S3 W1 17.5919.6 L5 16.6 S2 – W1 24 CAS 20.3 – CAS 24.8 L5 S1 W1–2 25.416.5 H5 22.2 S1 – W1 17.9 NU 16.1 – CAS 10.1 CK4 – – – – separate entry See CAS 20 H4 S2 W1 18.5 ± 0.478.3 H5 16.4 ± 0.3 – S1 W2 18.3 CAS 16.3 – CAS 11.5 H5 S2 W2 18.791.3 L6 16.5 S1 – W1 24.2 CAS 20.7 – CAS 342.5 H4 S1 W1 17.6 ± 0.3 15.9 ± 0.2 – CAS 123.6 L5 S2 W2 24.7108.2 21.3 L5 – S1 W1 24.6 CAS 22 – NU 166.1 L5 S1 W2 24.5 21.1 – NU 143.4 Ure – – – – separate entry See CAS 186.2 H5 S1 W2 20.2 18.3 – NU 32.2 H6 S2 W2 18.5 16.5 – CAS 1101.8 L4 S1 W1 21.6 ± 4.4 17.9 ± 1.8 – NU Mass (g) Class Shock WG ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ 15 06 57 32 56 37 13 41 25 42 27 55 17 15 47 30 56 40 47 15 31 01 45 20 20 20 07 23 15 23 48 13 48 24 49 18 08 21 17 03 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ 75°16 75°16 75°18 75°15 75°18 75°12 75°15 75°18 75°13 75°13 75°17 75°15 75°19 75°12 75°03 75°12 75°14 75°19 75°15 75°15 75°14 75°19 75°16 75°13 75°13 75°13 75°11 75°16 75°13 75°19 75°06 75°16 75°12 75°16 75°10 75°15 75°12 75°15 Longitude (E) 75°06 75°12 ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ 36 38 30 56 10 01 45 34 54 58 32 24 07 55 47 51 02 04 14 58 02 05 39 47 59 50 47 18 30 06 17 50 33 32 12 41 45 55 50 51 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ Latitude (S) Date found (mm/dd/yyyy) GRV 020158GRV 06/01/2003 72°58 GRV 020155GRV 06/01/2003 72°58 021496GRV 01/13/2003 72°56 GRV 020129GRV 06/01/2003 72°58 021493GRV 01/13/2003 72°56 GRV 020048GRV 01/01/2003 73°00 GRV 020116GRV 06/01/2003 72°58 021488GRV 01/13/2003 72°57 021581GRV 01/14/2003 72°57 GRV 020047GRV 01/01/2003 72°59 GRV 021487GRV 01/13/2003 72°56 GRV 020103GRV 06/01/2003 72°59 021481GRV 12/01/2003 72°56 021579GRV 01/14/2003 72°57 GRV 020039GRV 12/28/2002 73°09 GRV 020099GRV 06/01/2003 72°59 020297GRV 10/01/2003 72°59 021563GRV 01/14/2003 72°56 GRV 020029GRV 12/28/2002 73°04 GRV 020090GRV 04/01/2003 72°59 020283GRV 10/01/2003 72°59 021558GRV 01/14/2003 72°56 GRV 020025GRV 12/28/2002 73°04 GRV 020082GRV 03/01/2003 72°59 020236GRV 09/01/2003 72°58 021547GRV 01/14/2003 72°57 GRV 020017GRV 12/26/2002 73°05 GRV 020079GRV 03/01/2003 73°00 020226GRV 09/01/2003 72°59 021512GRV 01/13/2003 72°56 GRV 020015GRV 12/26/2002 73°07 GRV 020078GRV 03/01/2003 73°00 020200GRV 08/01/2003 72°59 021509GRV 01/13/2003 72°57 GRV 020013GRV 12/26/2002 73°06 GRV 020168GRV 07/01/2003 72°58 GRV 020075GRV 02/01/2003 72°59 021505GRV 01/13/2003 72°56 Name GRV 020010GRV 12/26/2002 73°06 Grove Mountains (GRV) Grove 020005GRV 12/25/2002 73°05 Table 4. Meteorites from Grove Mountains, Antarctica. Table Meteoritical Bulletin No. 89 A237 Type (MSU) Info 1.64 –1– La15 La15 1.68 –9.16 – La15 La15 Type (g) –CAS a a a a Fs (mol%) Comments Info 026 026 026 026 9.3 ± 5.5 (2.1–24.1) Fs (mol%) Comments Info Fa (mol%) Wo (mol%) Comment (2.3-16.2) Fa (mol%) Fs (mol%) Fa (mol%) 1.2 Ure – – – – See separate entry CAS 1.1 CV – – – – separate entry See CAS 4.7 L5 S4 W3 22.8 19.6 – CAS 5.1 L5 S4 W2 23.4 20 – CAS 73 L6 S4 W2 23.9 20.2 – CAS 24.9 Ure – – – – separate entry See NU 2.7 10.758.9 13.75 1 Pallasite 1 EL4 – LL5 L6 – B S4 S4 – B B B – 27.8 – 21.1 25.8 1.5 See separate entry 19.9 – Ha6 See separate entry – Ha6 Ha6 Ha6 274.1 L6 S1 W1 23.6 20.3 – CAS 442.6 CR2 – – – – See separate entry CAS 108.9 L5 S1 W2 25 25.9 – NU 67.6 1 L6 S4 B 24.9 21.8 – Ha6 44.2 1 LL5 S4 B 27.7 22.6 – Ha6 62.8 1 LL5 S4 B 26.8 25.9 – Ha6 19.5 110.9 1 LL512.2 LL5 1 S3 S3 B LL5 B 31.4 S4 27.6 26.4 B 24 – 27.3 – 22.4 – Ha6 Ha6 Ha6 2953 LL5 S2 W2 26.1 21.4 – NU 4360 H3 S1 W1 14.6 ± 3.5 Mass (g) Class Shock WG Mass (g) Pieces Class Shock WG 134.6 1 L5 S3 B 22 19.8 – Ha6 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ Continued. 00 11 37 10 01 20 37 36 47 01 51 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ 99.5 1 Lunar – – – – – Paired with Dho 36.7 131.5 173.1 Lunar – 1 Lunar – – Lunar – – – – – – – – – – – – Paired with Dho Paired with Dho Paired with Dho Mass (g) Pieces Class Shock WG 75°15 75°19 75°19 75°18 75°19 75°19 75°17 75°17 75°17 75°20 Longitude (E) 75°16 Long (W) 68°49.579 68°39.064 68°58.310 68°53.186 69°02.485 68°48.370 68°47.542 68°48.045 68°49.107 68°48.120 68°53.532 ′ ′ ′ ′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ 04 28 26 54 50 24 25 25 22 25 38 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ Longitute (E) 54°00.096 54°00.145 54°00.202 54°00.436 Latitude (S) Lat (S) ′ ′ ′ ′ Latitude (N) Date found (mm/dd/yyyy) Date found (mm/yyyy) Date found (mm/dd/yyyy) Name PCA 01031PCA 01034 01/2002 01/2002 85°39.211 85°41.096 PCA 01017 01/2002 85°41.561 PCA 01003 01/2002PCA 01006 01/2002 85°41.116 PCA 01014 85°41.011 01/2002 85°41.241 Pecora Escarpment (PCA) PCA 01001 01/2002PCA 01004 01/2002PCA 01010PCA 01011 85°39.966 01/2002PCA 01013 01/2002 85°41.059 01/2002 85°41.174 85°40.500 85°41.253 GRV 023771GRV 01/02/2003 72°59 GRV 022931GRV 01/22/2003 72°46 GRV 022459GRV 01/21/2003 72°46 GRV 022171GRV 01/20/2003 72°46 GRV 022021GRV 01/20/2003 72°46 GRV 021788GRV 01/20/2003 72°46 GRV 021711GRV 01/20/2003 72°47 GRV 021710GRV 01/20/2003 72°47 GRV 021603GRV 021615 01/17/2003GRV 01/20/2003 72°49 72°46 Name 021594GRV 01/17/2003 72°49 Dhofar (Dho) Dho 457 03/04/2001 18°14.901 Name Dho 458 03/04/2001Dho 459 03/04/2001 18°14.917 Dho 460 10/04/2001 18°14.914 18°14.965 Table 5. Meteorites from Pecora Escarpment, Antarctica. Table Table 4. Meteorites from Grove Mountains, Antarctica. Table Table 6. Meteorites from Oman. Table A238 S. S. Russell et al. Type (MSU) Info 3.03 –1.97 – La15 2.85 – La15 1.17 – La15 2.58 – La15 2.17 – La15 1.17 – La15 0.91 – La15 La15 10.1 – Vr5 Type (g) 208 – Vr1 a a a a a a a a with Dhofar 935 026 026 026 026 026 026 026 026 with Dho 927, Dho 1190 Wo (mol%) Comment Fs (mol%) Fa (mol%) 35.4 1 Lunar – – – – – See separate entry 7.4 – Vr4 33.7 1 Lunar – – – – – Paired with Dho 44.7 124.3 122.3 Lunar – 170.7 Lunar – 1 – Lunar –36.2 – Lunar – – 118.9 – – 1 – Lunar – – – Lunar – – – – – – – – – – – Paired with Dho – – Paired with Dho – Paired with Dho – – Paired with Dho – Paired with Dho Paired with Dho 67 1 L5 S4 W1 25.4 21.9 1.6 – 14 7.5 Vr2 21.6 1 Lunar – – – – – See separate entry 4.8 – Vr4 74 1 L6 S2 W3 23.5 22 1.4 – 15 7 Vr2 86 1 H5 S3 W3 18.2 16.4 1.6 – 20 18 Vr2 74 1 H5 S2 W3 17.5 16.3 1.1 – 15 9 Vr2 38 1 H5 S2 W3/4 19.6 17.2 1.2 – 8 4 Vr2 21.7 1 Lunar – – – – – See separate entry 4.8 – Vr13 68 1 H6 S1 W2 17.4 17.3 1.8 – 16.2 – Vr1 16 1 CM2 – – – – – See separate entry 4.3 – Vr5 45 1 H4 S2 W4 17.2 16.8 1.3 Possibly paired 702 1 L6 S2 W2 24.2 20.3 1.7 – 140.5 – Vr1 114550400 1 1 1 L4 H4 S2 H5 S2 S2 W2 W2 23.4 W3 17.9 18.2 19.8 15 17 1.4 0.6 1.2 – – Probably paired 32.3 191 – – Vr1 Vr1 69.2 1 Lunar –190 – 1 H3.9 – S4 W3 – 16.9–21.0 15.9–23.6 1.2 – – Paired with Dho 55 Vr1 247 1 L6 S3 W1 25.3 20.8 – – 23.5 – NAU 508 1 H5 S3 W2 18.2 17.3 1.3 – 219 Vr1 113166 1 1 L5 L5 S3 S1 W3 W3 24.6 25.5 22.5 21.6 1.4 1.4 – – 24 32 16 17 Vr2 Vr2 170158 1 1 L5–6 L5 S3 S3 W2 24.8 W3/4 23.9 22.4 21.6 1.4 1.7 – – 29 83 16 17 Vr2 Vr2 274 1 H6 S2 W0/1 18.3 17.8 1.4 – 86.2 – Vr1 212 1 H4 S1 W2 17.6 16.4 1.2 – 55.2 – Vr1 Mass (g) Pieces Class Shock WG 1592 4 H4 S2 W4 18.5 16.6 – – 23 – NAU 1248 1 LL5 S2 W3/4 26.7 21.8 1.5 – 108 94 Vr2 2412 1 LL5 S3 W1 27.8 22.9 1.6 – 384 Vr1 ′′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ 36.6 ′ Longitute (E) 54°34.6 54°33.5 54°23.2 54°46.2 54°39.4 53°59.868 54°00.113 54°00.145 53°59.662 54°00.377 53°59.772 54°00.046 53°59.525 54°39.8 54°34.7 54°33.8 54°51.38 54°57 54°34.5 54°07.2 54°11.8 54°24.2 54°45.9 54°32.2 54°43.9 54°24.2 54°14.1 54°35.7 54°40.7 54°46.9 54°13.9 54°45.7 54°08.0 54°45.2 54°33.9 ′′ ′ ′ ′ ′ ′ ′ ′ ′ Continued. ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ 11.3 ′ Latitude (N) Date found (mm/dd/yyyy) Dho 959Dho 960 08/11/2002 11/16/2003 19°23.2 19°23.8 Dho 957Dho 958 11/15/2002 09/11/2002 19°05.5 19°05.1 Name Dho 461 04/22/2001 18°14.682 Dho 462 04/22/2001Dho 463 04/22/2001 18°14.800 Dho 464 04/23/2001 18°14.808 Dho 465 04/23/2001 18°14.976 Dho 466 04/26/2001 18°14.833 Dho 467 11/07/2001 18°14.814 Dho 468 12/07/2001 18°15.226 Dho 923Dho 937 11/11/2002 18°15.390 09/11/2002 19°20.1 19°10.9 Dho 961 12/11/2003 19°23.9 Dho 938 11/15/2002 19°24.3 Dho 964Dho 965 2004 2004 19°07.56 19°09 Dho 939Dho 941 12/11/2002 11/14/2002 18°12.5 18°34.9 Dho 942Dho 943 11/15/2002Dho 944 11/15/2002 11/16/2002 19°10.0 19°03.1 19°14.6 Dho 945 11/11/2002 19°05.7 Dho 946 11/15/2002 19°09.9 Dho 947Dho 948 11/14/2002Dho 949 11/15/2002 11/16/2002 18°21.2 19°23.9 19°07.5 Dho 950 11/11/2003 19°19.5 Dho 951Dho 952 12/11/2002 10/11/2002 18°37.9 19°03.9 Dho 954Dho 955 11/14/2002 06/02/2003 18°32.1 19°03.3 Dho 953 11/16/2002 19°08.1 Dho 956 10/11/2002 19°13.0 Table 6. Meteorites from Oman. Table Meteoritical Bulletin No. 89 A239 Type (MSU) Info 10.2 – Vr5 10 – Vr6 21.9 – UCLA Type (g) 148 – Vr6 100 75 Vr2 42.5 36.1 Wo Wo 8.5 8.0 with Dho 927, 953 with Dho 987 with SaU 064 Wo (mol%) Comment Fs (mol%) Fa (mol%) 4.57 1 Lunar – – – – – See separate entry 1.19 – UWS2 8.1 1 H5 S2 W3 18.5 16 – – 2.4 – NAU 24 1 L6 S4–5 W3 23.1 19.8 1.7 CaPx:Fs 14 – H6 S3 W3 17.6 15.1 1.5 – 12 – Vr6 12 1 LL6 S3 W5 28.5 23 – – 3.2 – NAU 82.6 1 H6 S3 W5 17.9 16.1 – – 16.6 – NAU 5893 1 1 H5 Acap S3 – W1 – 19.7 – 17.2 – – – – See separate entry 19 12.5 – – MNHNP MNHNP 35 1 H4 S3 W3 18.3 18 1.3 Probably paired 33 1 H4 S2 W4 17.5 15.6 – – 7.6 – NAU 79 1 LL4 S2 W2 26.1 23 – – 50.8 – NAU 79 1 H4 S1 W2 18.4 16.5 – – 17.8 – NAU 81.4 3 R3 S2 W3–4 38 ± 9 17 ± 6 – – 16 – Mün 124 1 H4 S1–2 W3 15.6 14.1 ± 1.6 1 – 46.6 – Vr6 422 1 L6 S4 W2 24.4 21 1.4 CaPx:Fs 650 Many H5 S3 W4 18.1 16.0 ± 4.5 0.1–1.1 – 220 – Vr6 174 1 L5 S2 W2 24.7 21.2 1.5 – 44.7 – Vr1 213.9114.5 1 1702 L6 Many H3.8 S3 H3 S1 S2 W5 W4 24.8 ± 0.4 17.3 ± 0.1 W3 – – 2.3–27.7 5.3 – – – – – – 31.61 25.59 – – 21.5 – UCLA UCLA MNB 608.5165.3 1 1 H6 H4 S2 S2 W2 W5 27.4 17.6 ± 0.4 – 22.8 – – – Possibly paired 28.8 – NAU 868 17 L5 S3 W4 24.6 21.1 – – 29.1 – NAU 499 1107.6 L7 1420 S2 H5 1 W4 S2 24.8 Ure W4 – 21.1 18.5 – 3.6 16.3 – – See separate entry 59 – – – Vr5 – – 20.2 – NAU 63.8 – Vr3 466 1 L6 S1 W3 22.8 20.5 1.2 – 47.8 – Vr3 146 1570 Many H5 H5 S2 S3 W2 W4 17.8 17.7 15.6 15.3 0.9 – – – 32.3 236 – – Vr6 Vr6 2467 1 L4 S2 W2 23.4 20.1 – – 30.5 – NAU Mass (g) Pieces Class Shock WG 2717 4 LL5 – W2 ± 0.3 29.6 24.4 ± 1.9 1.53 ± 0.2 – 20.1 – 14 Vr 1063 1 Ure S2 – – – – See separate entry – NAU 1728 1 H3 S1 W2 16.9–18.5 14.2–17.7 – – 89 – NAU 5079 52 Ure – – – – – See separate entry 640 – Vr3 1913 1 H6 S4 W2 18.2 17.1 1.3 impact melt With 637 – Vr1 745 1 H5 S2 W3 18.4 17.6 1.4 Probably paired ′′ ′′ ′′ ′′ ′′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ 22.3 00.5 34.6 00.5 0.96 ′ ′ ′ ′ ′ 54°21.84 54°56 Longitute (E) 54°22.41 54°35.96 54°21.982 54°50.14 54°43.77 54°53.65 54°39.676 54°05.81 54°54.36 54°55 54°50.17 54°56.2 54°57 54°59.13 54°22.624 54°03.40 54°44.8 54°05.400 54°33.8 54°55.03 54°55 54°56 55°06.91 55°02.39 54°28.371 54°38.37 54°50.02 56°15.9 56°6.955 54°46.507 57°19.53 56°29.01 57°16.8 57°19.1 ′′ ′′ ′′ ′′ ′ ′ ′ ′ ′ Continued. ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ 43.6 03.8 16.3 03.8 ′ ′ ′ ′ Latitude (N) Date found (mm/dd/yyyy) Dho 1195 04/18/2004 19°1.89 Dho 1197 12/04/2004 18°55.46 Dho 979 2004 19°45.4 Name Dho 966 2004 19°11.53 Dho 1196 04/13/2004 18°57.646 Dho 1191 11/11/2003Dho 1193 04/13/2004Dho 1194 11/04/2004 19°20.4 18°51.49 19°1.006 Dho 1221 2003 18°13.850 Dho 991Dho 992 2004Dho 993 10/01/2004Dho 996 10/01/2004Dho 1113 02/20/2003 19°19.07 2004Dho 1190 19°13.49 19°15.48 11/16/2002 19°9.819 19°08.2 18°08.53 Dho 983Dho 984 2004 2004Dho 990 10/01/2004 19°10.27 19°15.19 19°11.84 Dho 978 2004 19°13 Dho 968 2004 19°17.8 Dho 1222 2003Dho 1223 02/25/2004 18°45.645 18°12.25 Dho 989 2004 19°14 Dho 977 2004 19°13 Dho 972 2004 19°23.11 Jiddat al Harasis (JaH) JaH 054JaH 075 01/15/2004 2004Ramlat as Sahmah (RaS) 19°37.82 RaS 007RaS 008 01/02/2004 01/02/2004 19°14.78 20°10.2 20°43.679 Dho 1275 06/02/2003 18°49.71 Dho 1224 09/28/2003 19°19.605 Dho 974 2004 19°14 RaS 009 09/04/2004 20°2.81 SaU 172 11/17/2002 20°59.6 Sayh al Uhaymir (SaU) SaU 170SaU 171 02/22/2004 11/17/2002 20°57.96 21°00.8 Table 6. Meteorites from Oman. Table A240 S. S. Russell et al. Type (g) Info Type (MSU) Info 26.3 – Vr5 Type (g) 170 – Vr6 Place purchased Rissani 25 Asu1 Morocco 5.7 NAU ; Si in a 92.1–94.4 97.7 kamacite 2.1–2.5 wt% with SaU 067 1.6 ± 1.6 0.1 Wo – Rissani 50 Asu1 Wo (mol%) Comment 19.9 ± 0.4 21.65 ± 0.4 Fs (mol%) Comment PMD = 1.8 PMD = 1.7 Fs (mol%) Fa (mol%) PMD = 2.3 PMD = 4.2 Fa (mol%) – – – – See separate entry – 22 Be2 anomalous Weight (g) Pieces Class Shock WG 38.5 3 H5 – W4 ± 0.2 18.3 18.6 ± 1.6 1.47 ± 0.7 – 7.8 – Vr14 556 1 L4 S2 W2 24.4 21.6 – – 28.8 – NAU 802120 1 1 H4 EH3 S2 S4 W3 W1 17.6 0.4 15.9 1.6 1.2 0.7 – En 184 – Vr1 622 5 L6 S1 W2 23.7 21.2 1.2 – 27.5 – Vr3 207 1 L6 S4–5 W3 22.7 18.6 – – 44 – Vr6 690 1 L6 S4 W3 22.8 18.6 – Possibly paired 2579 2 L5 S3 W1 22.7 19.1 1.5 sv 104 – Vr6 Mass (g) Pieces Class Shock WG ′′ §4.2b. See Warren (2005). §4.2b. See Warren ′ ′ ′ ′ ′ ′ ′ Longitude (W) 45.5 ′ 56°40 56°31.190 53°53.16 53°58.3 53°52.9 56°42.154 Longitute (E) 57°17.954 57°17.85 Latitude (N) ′′ ′ Continued. ′ ′ ′ (uncertain locations; numbered). ′ ′ ′ 53.4 ′ Latitude (N) lature Committee guideline Date found (mm/dd/yyyy) P2001 – – 1440 1 L6 – W3 25 – – Tucson 20 MK2 Possible or origin pseudonym –– 2002 2002 – – – – 20.2 28.8 1 1 Ure Euc S2 S4 W1 W1 12 – 12 42–52.4 Plag An – Morocco 4.2 NAU Morocco Date found (mm/dd/yyyy) b b r 012 12/11/2002r 013 06/04/2004 18°33.7 18°29.5 r 014 04/14/2004 18°19.73 ∫ ∫ ∫ NWA 1835 NWA Name NWA 1697NWA Morocco 1809NWA 1834 NWA 2002 – – – – 3000 – 1 L5 214 S4 1 W1 LL6 23.9 ± 0.6 S2 W2 23.5 30.3 – – 20.7 Prato3 NWA 1696NWA Morocco 2002 – – 213 1 L3-6 S1–3 W1 25.9 ± 0.7 Northeast Africa (NEA) NEA 001Northwest Africa (NWA) Sudan 484NWA 774NWA – 04/2002 775NWA Morocco Southern P2001 – P2000 – – – – – 262 1 523 Lunar 98 1 1 – H4 H5 – – – – W2 18 W1 19 – – See separate entry – – – – 20 PCU1 Tucson Erfoud 20 MK2 20 MK2 NWA 903NWA 1052NWA – 1054NWA Morocco 1329NWA Morocco 2001 1337NWA – 2001 1356NWA – 2003 1390NWA – 1392NWA – – 1392NWA – P2000 – 1395NWA – P2000 – 1397NWA – P2000 1406 –NWA – P10/2000 – 1429 –NWA – P10/2000 – – 1628NWA – P10/2000 – – 1665NWA – P10/2000 – – Morocco P10/2000 – – P2001 22 – 2002 – – P2001 86 >529 – – 2003 1 – Several 1 – – H3 465 – – Acap – 92 Acap 270 1 – 76 1091 – 1 S1 – – – 1 64 1 H4 3 – 734 40000 – W3 L3.9 – 1 H3.8 H5 1 L6 1 – 14.85 682 – 1185 H5 – – 62.6 H3.8 – L/LL6 1 – – W2 1 18.2 – 1 – W3 W1 – 1 19 – LL3 – W1 CK3 18 L3 W4 – 8.2–18.1 19 CK W3 – – W1 25 W1 – 24–27 – 18 19 – – See separate entry – S4–6 W2 See separate entry Erfoud W2 W1 – – 85–1 Erfoud – 3–6 br, – 65–1 Erfoud – – – – 4.7 – – 17.9 – – Prato4 Prato3 28.9 Morocco – – – Prato3 – Morocco 56 analyses 20 Morocco – Morocco MK2 See separate entry Morocco 20 Morocco Morocco 20 Rissani Morocco Morocco MK2 15 20 MK2 20 20 MK2 13 20 MK2 MK2 7.8 Morocco MK2 NAU MK2 MK2 13 MK2 SaU 183 02/21/2003 20°10.572 Shi Shi SaU 180 2004 20°32 Shi SaU 175 01/02/2004 20°34.38 Name SaU 173 08/04/2004 21°3.31 SaU 174 08/04/2004 21°3.867 Formal pairing under Nomenc Table 7. Meteorites from Africa Table Table 6. Meteorites from Oman. Table a Meteoritical Bulletin No. 89 A241 92.6 Asu1 Type (g) Info Rissani 17 Mün3 Place purchased Morocco 25.5 NAU Rissani 25Rissani Ha3 21 Mün3 a 91–93.6 ; pbr Rissani 17 Mün3 ; mbr Marie St. 14 Mün3 1.2 ± 1.3 0.3 90 ± 2 90 84–97 84–93 impact melt br 42 ± 13 An Fs (mol%) Comment Fa (mol%) 28 – – – – See separate entry – 21.1 NAU achondrite Continued. Weight (g) Pieces Class Shock WG Longitude (W) Latitude (N) – – 222.6 1 H4 S1 W5 18.8 ± 0.2 – – 21.1 UCLA (uncertain locations; numbered). Date found (mm/dd/yyyy) Fall/Winter 2002 200220022002 –2002 – –2002 – – – – – 104.1 – 1 316 – 282 1 H3 1 70.8 H3 316 1 S1 LL3 1 W2 H6 S1 S4 17.4 ± 0.4 L6 W5 S2 W3 17.3 ± 0.4 – 23.5 ± 12.9 S4 W2 – 18.9 ± 0.2 – – W2 24.5 ± 0.3 – – –02/2002 –06/2003 – – – – – – – – – 26 – UCLA 39.4 – 35.8 94.2 UCLA 16500 UCLA 1 16.12 1 UCLA L5 20.88 L/LL4 UCLA – – W1 W1 24.7 25.9 21.7 22 – – Hamburg Margarite Ste. 20.2 20.5 Bart3 Bart2 Possible or origin pseudonym – 2002– –Morocco 2003Morocco –Morocco –Morocco 1102Morocco – 1Morocco Euc 32.3 S 1 W0 Ure – – 56.4–59 1 Plag An 0.8–21.8 18.3 –Algeria Algeria Morocco 8.4 NAU b b NWA 1841 NWA NWA 1842NWA 1852NWA – Eastern 1853NWA Eastern 2003 – – 70.5 1 L4 1967NWA 1968 S2NWA – 1969NWA – 1970NWA W2 – 1971NWA – 23.6 1972NWA – 01/2003 – 01/2003 01/2003 – 01/2003 21.6 – 01/2003 – 01/2003 – – – 2020NWA – – Morocco/ – – – – – 82.9 80.4 1 Erfoud 74.4 1 68.5 1 L6 66.2 1 L6 64.2 14.1 1 L6 NAU 1 H5/6 S4 L6 S3 LL5–6 S2 W1 S2 W0/1 S4 25 S4 W1 25 W3 25 W2 W1 18.5 30 25 21 21 16 21 sv 24.5 21 sv – – fragments of sv, br, – Rissani Rissani Rissani Rissani 17 18 Rissani Mün3 15 Mün3 17 Mün3 Mün3 14 Mün3 Name NWA1836 1837NWA 1838NWA – 1839NWA – 1840NWA – – 2003 2003 2003 2003 – – 1854NWA – Eastern 1855NWA – – Eastern – 1856NWA – Eastern – 1857NWA Eastern 1952NWA 45 1955NWA Morocco 22.1 121.8 Morocco 1 1 2001 132.8 1 2002 1 H4 L3 L7 – Enstatite – S2 S1 – – W1 – W1 – 17.9 24.9 – 636 2000 16.1 21.1 1 Several H/L3–4 – L6 – – – – S3 See separate entry – 20.6 W5 Erfoud 2033 ErfoudNWA 26.6 Morocco/ 20.44 9 20.1 4.6 – NAU NAU NAU Wo – Rissani 20 UCLA NWA 1973NWA 1974NWA – 1975NWA – 1976NWA – 1977NWA – – 01/2003 01/2003 01/2003 – 06/2003 – 06/2003 – – – – – – – – 57.2 39.1 1 28.4 1 65.7 1 L6 69.1 1 LL4/5 1 L6 L(H)3 S2 S4 Euc S2 W2–3 S3 W1 28 S4 25 W3 W1 14.5 ± 8 W1–2 25 – 23 21 ± 8 11 21 – – 61.1 ± 1.5 partly S5 sv, An – Rissani Ensisheim Rissani 13 14 Mün3 Rissani 8 Mün3 Mün3 6 Mün3 NWA 1957NWA – 1962NWA 2002 1963NWA – 1964NWA – 1965NWA – 1966NWA – – – 01/2003 01/2003 01/2003 – – 01/2003 – 01/2003 – – – 6593 – – – Several – L5 – 150 146 S1 140 1 118 1 W2 1 85.5 H5/6 1 L6 24.7 ± 0.5 4 L6 S4 H3–5 20. 5± 0.4 Euc Wo S2 W1 S2 S2 19 W1 S2 W2–3 W3 25 24 W2 16.5 ± 8 2 grains: 26; 17 13.5 ± 5.5 21 20 br sv – – Rissani Rissani Rissani 21 Rissani 23 Mün3 Mün3 23 20 Mün3 Mün3 NWA 1958NWA 1959NWA – 1960NWA – 1961NWA – – 01/2003 01/2003 01/2003 – 01/2003 – – – – – – – 244 209 206 2 288 1 1 L6 3 LL6 H5 Mes S4 S3 S2 W3 S2 W1 26 W2–3 29 W0/1 18 1 grain: 36.0 32.0 ± 2.0 An 22 24 16 calc.v. sv, calc.v. sv, – Rissani Rissani 22 Rissani 23 Mün3 Mün3 24 Mün3 Table 7. Meteorites from Africa Table A242 S. S. Russell et al. Type (g) Info ErfoudErfoud 3.7 Prato3 20.3 NAU Erfoud 8.1 NAU Rissani 88.5 NAU Place purchased Erfoud 1.7 UWS RissaniRissaniRissani 7.6 22.7 NAU 42 NAU NAU Erfoud 14.4 NAU8 Erfoud 20 UWS ; to 0.3 34.2 Or Wo a 26 0.1 84.3 91 Or 2.1 7.3 88.8 = 26.2–30.3 An subtype 3.8/3.9 FeS rimmed by NiFe disk-shaped separate entry Cr/(Cr + = 1.0 Al) plag An Fs (mol%) Comment Mean = 24.9suggest data Olivine Fa (mol%) Mean = 35.6 Continued. Weight (g) Pieces Class Shock WG Longitude (W) Latitude (N) (uncertain locations; numbered). Date found (mm/dd/yyyy) 04/2003 – – 114.6 1 H5 S2 W4 18.4 16.4 – – 33.5 FSAC 1 Possible or origin pseudonym –– 2002 2002 – – – – 8.4 800 1 1 Dio– Dio– – – 10/2003 – 10/2003 – – –– – – – – 22.3–22.6 11/2003 Plag: An 24.2–24.3 FeO/MnO – 114– 33 2 – 1 2003 Dio Ure 252 – – – 1 W0 – – Ure 6.9 4–17.8 S3 23.3 67 15.6–10.1 W2 – 1 mbr 7.8–10.3 Euc 9.1 S2 Rissani Rissani Wo W1 22.2 – 8.5 NAU NAU 46.5 Augite Fs (Desert) b b b b b b NWA 2038 NWA NWA 2082 NWA 2083 NWA 2084 –NWA 2085NWA – – 10/2003 10/2003 10/2003 – – – – – – 144 786 2700 1 1 1 CO3 LL3.8 L S1 S2 W2 S6 W2 3.8–57.6 29.7 – – 22.8 24.2 – – – melt rock; see Rissani Rissani 24.5 28.8 NAU NAU Name 2037 NWA 2042NWA 2045NWA Morocco – 10/2003 – 2003 – – – 700 1 Mes 19 1 – LL3 – S2 – W3 29.8–43.7 – See separate entry Erfoud 20 UWS NWA 2055NWA 2056NWA – – 2057NWA 2069NWA – – 2070NWA – – 2071NWA – 2072NWA – 2073NWA – – 2074NWA – 2003 – 2075NWA – 2002 – 2076NWA – 2002 2077NWA – 2002 2078NWA – – – 2002 – – – – 2002 2081 NWA – 2002 – 2002 – – – 2002 – 148 – 2003 – 1447 – – 1 – – 2086NWA 1 – – 2087NWA 958 – 44.9 – – H4 – 90 L4 1 – 816 1 – 1 1 – 1 R 11/2003 H4 S2/3 8.1 174 11/2003 S3 1 H4 484 W1 1 H4 338 1 – W2 18.0–18.4 1 – L5 S2 S2 H4 1 1 20.4–23.6 34.8 L5 S5 16.6–17 S1 W2 W3 – L4 1 1 20.8 – L5 W1 S3 18.4 39.1 W1 S2 S2 H4 18.6 H5 17.9 W2 S1 clasts; 5 mm Melt W1 S3 W2 780 23.5 16.3 18.1 W2 – S2 S2 35.1 23.4 16.5 Many W2 16.2 24.6 1 CV3 Zagora – 25.5 W2 W1 20.8 16 – Shock darkened 18.3 18.5 – 20.8 H5 S1 21.4 Erfoud 21 – 22 – W1 – NAU S2 16.5 16.7 – Erfoud 18.8 1.8–41 – W1 Erfoud NAU Erfoud – oriented, 18.8 3–35.5 21 Erfoud Erfoud 23.2 Erfoud – 22.4 NAU Erfoud NAU 16.6 NAU 26.7 Erfoud 22.2 NAU 8.1 Erfoud 20.4 Wo NAU NAU NAU 24.2 Rissani 21.8 NAU NAU 28.1 NAU NWA 2088 NWA 2089 NWA – 2090NWA 2091NWA – 2092NWA – 2110NWA – 11/2003 2111NWA – 2112 NWA – 11/2003 – 11/2003 2114NWA 11/2003 2152NWA – – 2003 2153NWA Morocco – 2003 – 2154NWA Morocco – 01/2004 2155NWA Morocco – 01/2004 2156NWA Morocco 2003 – – 01/2004 2157NWA Morocco – – – 01/2004 Morocco 429 – 01/2004 – – – – 875 – 1 – 580 – – 320 1 – LL3 – 1 – 1 – 28 CO3 984 226 LL4 S2 353 1 LL6/7 1 233 1 S1 W2 89 1 35.8 S2 CV3 S3 1 L4 27.6 W1 27 L5 1 1 W2 L6 W1 12.2–53.2 1 LL6 S2 29.1 L6 L3.9 30.9 S2 23.4 S4 – W4 L6 S4 S4 W2 W2 S2 1.7–39.6 S4 24.4 Chromite; W1 24.7 23.7 W2 24.2 – W1 S3 24.1 W1 – 30.5 – 20.4–25.1 – W0 23.7 20.6 20.1 23.9 – 20.2 – 24.9 – 20.2 Rissani – sv 20.1 – – Rissani Rissani – 40 – Erfoud NAU 47.5 25.7 Erfoud NAU – NAU – Erfoud – 2.4 – 27.8 NAU1 – NAU1 20.4 24.7 24.9 NAU1 Be8 22.6 Be8 Be8 7.2 Be8 5.5 Be8 Table 7. Meteorites from Africa Table Meteoritical Bulletin No. 89 A243 Type (g) Info –9.6FSAC 1 –9.6FSAC – 12.6 FSAC 2 Place purchased ErfoudErfoud 30 40 Mün7 Mün7 a 91 ± 2 91 NWA 2159 NWA with Sahara 02500 An 84–95 6.1–21.0 – Erfoud 29.4 Prato3 20.9 possibly paired br, Fs (mol%) Comment peak: 36 ± 1.5 13.5 ± 4.5 sv br, Munich 17 Mün3 Fa (mol%) Mean = 6.7 (20–26) Continued. Weight (g) Pieces Class Shock WG Longitude (W) Latitude (N) (uncertain locations; numbered). Date found (mm/dd/yyyy) 04/2003 – – 31.3 1 L5 S3 W2 25.5 21.9 Possibly paired with 04/200304/2003 –04/2003 –04/2003 – –04/2003 – –04/2003 – –04/2003 569.9 – – 1 417.2 – – 1 – LL4 63.506/2001 1 – H5 57.106/2001 – S2 1 54.906/2001 L5 – 1 W4 18.4 S12003 L5/6 – – 1 28.1 W4 L5 5.4 S3 – S4 1 18.5 H4 – W1 – 23.2 W3 – 24.7 H5/6 13 kg Many 25 – – 16.3 300 W4 – LL6 – 700 3 21.42002, found 26 W4 – – 1 W4 18.9 S3 18.3 LL5 367.2 – 18.2 Several W2 L5 H3 22.6 – – – 27.2 S1 16.1 16.4 – – W4 S2 S1 – 25.6 23.7 – W2 W2 129.9 br 32 – FSAC 1 24.2 0.8–18.4 – 1 22 21.8 – FSAC 1 LL4–6 16.3 – 20.7 – FSAC 1 – 11.9 S2 FSAC 1 br – W3 14.4 FSAC 1 29.5 4.1 1.6 FSAC 1 – FSAC 1 25.49 24 – UPVI 23.48 calc.v. sv, br, UPVI 29.01 UPVI Morocco 6.5 Mün3 04/200304/2003 – – – – 9.6 1 89 1 L5 L5 S2 W2 S3 25.5 W2 25 22 21.8 – – – – 3.2 FSAC 1 32.6 FSAC 1 Possible or origin pseudonym (Desert) (Desert) (Desert) (Desert) (Desert) (Desert) (Desert) (Desert) (Desert) (Desert) (Desert) Africa (find) (Desert) (Desert) NWA 2159NWA Morocco Name 2158NWA Morocco 2160NWA Morocco NWA 2161NWA Morocco 2173NWA Morocco 2181NWA 2182NWA – 2183NWA – 2184NWA – 2185NWA – 2186NWA – 10/25/2002 2187NWA Touz 10/25/2002 2188NWA – – 10/25/2002 2189NWA Morocco – 10/26/2002 2002 Boudnib – 10/25/2002 Unknown – – – 2002 – – – – – – – – 448 – 104 1 56 – 1 83 96 1 L6 129 1 H5/6 316 1 H3–5 1 1 H3–5 308 S3 S2 H4 H4 S2 1 H5/6 W3 W1 S2 W1–2 26 17.5 S2 CO3 19 ± 2 W1 S2 S1 18.5 W2 W3–4 W2 S2 16.5 15.5 17.5 17 21.5 18 W1 br – 18 ± sv 15 ± 1.5 15 16 calc.v. 4 ± 2 – – – Munich Munich Munich Morocco 11 21 19.5 29 Mün3 Mün3 Munich Mün3 Mün3 Marie St. Marie St. 21 25 24 Mün3 Mün3 Mün3 NWA 2162NWA Morocco 2164NWA Morocco 2165NWA Morocco 2167NWA Morocco 2168NWA Morocco 2169NWA Morocco 2170NWA 2171NWA Erfoud Erfoud 05/2003 2174 05/2003NWA Morocco 2175NWA – – Morocco 2179NWA Northwest – – 480.3 13.5 1 Many L3.8 LL6 2193NWA 2195NWA – 2196 S4NWA S2 – 2197NWA – 2198NWA W1 – W1 2199NWA – – 24.0 25.4 2226NWA – – – – 01/2002 01/2002 22.6 01/2002 – – – – – – – – – – – – – – – 785 293 – – 152.5 141.7 1 38 2000 1 1 1 1 1 L6 LL3.6 LL3.7 1004 CR2 24.2 R4 H FSAC 2 S2 1 S2 S3 S1 W4 W3 How W3 S2 S6 W5 17–29 24.4 9.0–23.0 W1 W2 – 1.0–2.4 38.5 – 18.6 – W1 – – – – – – – – – – 26–51; Melt breccia Erfoud – – – – 20 Erfoud UCLA 21 20 24.1 21 UCLA 8 UCLA UCLA UCLA UCLA NWA 2227NWA – – – – 302 1 Euc – W3 – 45–58 Impact melt br; An: Table 7. Meteorites from Africa Table A244 S. S. Russell et al. Type (g) Info – 20.8 MNHNP Place purchased – 20.5 Vern ; a 0.4‰ 85–94 − O = 17 Ni, Ni/Co 7.2 Ni/Co Ni, ∆ ––5.6Be5 – –– 17.8 Be5 – 24.1 Be6 6 7. 14.6 Fs (mol%) Comment (1.7–17.1) (6.6–18.2) (0.4–18) Fa (mol%) (0.4–28.1) (4.5–21.4) (2.7–25.6) Continued. 80.5 1 L447.957.4 1 159.3 S2 L661.8 1 L6 1 W1 L540.2 25 S3 L640 1 S333.9 W224.5 1 1 S3 W2 L6 24 1 S3 22 24.5 L3.8 W2 L3.8–6 W4 L3.8 24 S4 S3 24.7 – S3 20 20 W3 S2 W1 W1 25 20.5 24.5 ± 8 W1 20.6 24 ± 10 – – 25 ± 11 23 ± 13 – – 24.5 ± 14 – 23.5 18 ± 6 – br – – – – 25.5 – Pa14 – – – 24.2 20.4 – – Pa14 Pa14 21.5 20.6 Pa14 21.1 Pa14 20.4 Pa14 Pa14 20.2 18.2 Pa14 Pa14 65 1 Euc – – 71 16–61 Plag An 129.5110.7 1215.4 1 1 L5 L5485 H5 1 S3139 S4135 H5 S4 W3 1 W4 1 23.5 W2 25 L6 S4 18 L6 W4 22 S4 24 18.5 S4 16 W3 – W3 25 – 17.5 25.5 – – 21.5 24 – – – – – – 23.6 Pa14 23.7 26.3 Pa14 – Pa14 – 28.4 Pa14 26.7 24.6 Pa14 Pa14 184 1 CV3 – – – – See separate entry – 23.6 MNHNP Weight (g) Pieces Class Shock WG ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ 7°57 17 1 How – – – 43–53 separate entry See – 16 Pa14 7°45 7°47 7°40 7°54 7°58 7°59 7°54 7°51 7°57 7°50 7°30 7°32 7°35 7°31 7°54 7°51 65 1 H6 S1 W3 19.5 16.5 – – 20.89 Pa14 Longitude (W) 7°53 7°57 ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ ′ Latitude (N) (uncertain locations; numbered). Date found (mm/dd/yyyy) 10/2001 27°58 Algeria Possible or origin pseudonym – 2003 – – 167 1Algeria Ure 09/2002 – 28°14 – 20.3 76.4 Rare metal: 2.25% b b NWA 2251NWA Tindouf, NWA 2254NWA 2255NWA Algeria 2256NWA Algeria 2257NWA Algeria 01/02/2000 2258NWA Algeria 01/16/2001 2259NWA Algeria 28°12 01/07/2001 2260NWA Algeria 27°56 01/10/2001 2261NWA Algeria 27°46 01/11/2001 2262NWA Algeria 28°30 01/06/2001 2263NWA Algeria 28°35 01/11/2001 2264NWA Algeria 28°36 01/09/2002 2265NWA Algeria 27°56 01/10/2001 2266NWA Algeria 27°44 01/01/2002 2267NWA Algeria 27°48 01/05/2002 2268 NWA Algeria 27°49 01/04/2001 27°55 01/03/2001 28°40 01/09/2002 28°45 28°06 NWA 2253NWA Algeria 01/11/2000 28°10 Name 2233 NWA 2252NWA Algeria 04/04/2002 27°49 NWA 2269NWA 2271NWA Algeria 2272NWA Morocco Morocco 10/2001 2273NWA 2003 2274NWA 2003 Morocco 2275NWA Morocco 27°58 2003 2276NWA Morocco 2003 2277 –NWA Morocco 2003 2278 –NWA Morocco 2003 2279NWA Morocco – 2003 Morocco – 2280 –NWA 2003 – 2282 –NWA 2003 Morocco 2283 –NWA Mauretania – 2003 2284 –NWA 2003 Morocco – 2285 –NWA Morocco – 434 2003 2286 –NWA Morocco – 22 2003 2287NWA Morocco – 1 – 2003 2288 –NWA Morocco – 39 2003 2289 1NWA Morocco – 15 – 2003 2290 L6NWA Morocco 164 1 – 410 2003 2291 –NWA Morocco – L3 1 – 1694 2003 Morocco 1 2292 –NWA 2003 – 1 H6 62 S6 2293 –NWA 2003 Morocco 1 – L6 85 – H5/6 Morocco – S2 L6 2003 1 – W0 – 147 155 H4 2003 1 – S2 – W1 23 – S2 S4 – 106 1 L6 1 W3 12.2 – Ure S6 45.9 – W2 W1/2 – S2 126 1 – L6 18.1 L6 1 – 23.5 W1/2 82 17.2 S4 19.5 W3 1 49.8 23 L6 S0/1 – 150 L5/6 1 – 16.9 1 W3/4 160 W2/3 S5 15.9 S6 L6 19.8 Partly melt rock 134 23.4 1 14.2 15.4 Dio 300 1 S4 W2 L6 S4 W3 19.8 – 1 – L3 15.4 350 – 23.7 1 S6 22.2 W2 – W3 R3–6 107 20.5 Mod. LL6 1 Partly melt rock 23.3 S4 22.5 W0 L/LL3 – – 1 S3 – 20.2 – – 20.3 18.3 W1 24.3 H4 S3 26.8 S3 W2 L4 Be5 25.9 20.1 – 19.6 – – W2 – – W2 Partly melt rock 1–35.3 17.4 S2 29.3 – 21.9 19.1 – S4 – – 24.4 – 20.8 W3 1.9–28.5 Be5 – Partly melt rock W2 17.5 – See separate entry 9.6 5.8 24.1 20.6 – 23 – Be5 – – – Be5 Be5 23.1 24.9 br 15.9 – – Be6 15.2 Be5 See separate entry 19.5 Be5 21.3 – – – 23.5 22 – Be6 Be6 – Be6 20.5 9.4 – Be6 Be6 24.4 20.7 11 Be6 Be6 – Be6 – 24 Be6 25 21.6 Be6 Be6 Table 7. Meteorites from Africa Table Meteoritical Bulletin No. 89 A245 Type (g) Info Erfoud 21.1 NAU3 Erfoud 28Erfoud NAU5 22.8 NAU1 Place purchased –3.7Be2 –44Be8 ErfoudErfoud 11.2 NAU4 21.1Erfoud NAU4 22 NAU5 ; a ; ; ; 12.5 83–91.5 81.3–94.9 88.9–92.1 91.5 89.2 9.4 ; pbr Wo Wo 6.5–40.3 6.3–43.9 O = –1‰ 81.6 11 46.4 17 1 cm – – 20 Be7 Fs ∆ Pigeonite Fs An Plag An Plag An > 13.7 (6–19.9) Fs (mol%) Comment Fa (mol%) (2.5–24.2) Continued. Weight (g) Pieces Class Shock WG Longitude (W) Latitude (N) (uncertain locations; numbered). Date found (mm/dd/yyyy) 2002 – – 18 1 Euc – – – 29.7–58.5 Wo Possible or origin pseudonym Sa- Western hara Morocco 2004– – 2004 –– –– 1905 2004 – 1 2004– – Euc 302 – –– 2004 – 1 – – Ure – 2004 53 – – 1 – 1298 – 1– – Euc 23.1–55 – Euc Wo 10.7–11.9 252 – 2004 1 – – – 1239 Euc – – 4 Pigeonite – – Euc – – – 37.1–43.1 – Plag An 54.6 31 – Plag An 1 – 59.3–62.9 Ure Plag An – – – 56.4; 43.9; 59.0 12.9–21.0 – – Erfoud 6.7 NAU5 b b b b b b b b NWA 2375NWA – 2004 – – 544 1 L5 S5 W2 23.7 20.1 Shock darkened Erfoud 29.2 NAU1 Name 2294NWA Morocco 2295NWA 2003 2296NWA Morocco Morocco 2297NWA 2003 2298NWA Morocco 2003 2299NWA Morocco – 2003 2300NWA Morocco 2003 2301NWA Morocco – 2003 2302NWA Morocco – – 2003 2303NWA Morocco – 2003 2304NWA Morocco – 2003 2305 –NWA Morocco – – 2003 2306 NWA Mauretania – 2003 – 2003 984 – – – – 1 – – 858 3600 – – – 1635 H3 – 1 1 – 474 3826 1 – – L6 L6 144 1 S2 1 167 L6 1 50.9 W1 L6 3435 S4 1 L5/6 S4 7500 1 19.4 940 L3 1 S4 W1 W1 L3 1 S4 S4 H5 1 23.6 W2 23.2 L6 L5/6 S3 W1 W2 23.2 L5/6 S3 S3 23.1 22.9 W0/1 20.4 19.8 S4 S4 W1 13.6–24.4 S2 W3 19.6 W1 W2 – 2.5–27 16.3 – 19.7 19.6 6.2–20.5 W1 23.5 23.3 – sv 23 2.3–20.5 – – 14.8 – 19.8 19.7 – 19.6 – – – – – – – – – – 23.3 20.1 Be7 22.1 Be7 22.6 – – Be7 Be7 – 31.8 23 21.6 – Be7 Be7 Be7 13.1 27.8 20.4 Be7 Be7 22.2 Be2 Be2 NWA 2353NWA 2354NWA – 2355NWA – 2356 NWA – 2004 2002 2002 – – – – – – 2367NWA 2368NWA 315 – 2369NWA 727 – 286 – 1 2370NWA 1 2371NWA – 1 2004ung Achond 2372NWA – 2004 – H5 2373NWA – 2004 LL5 2374 NWA – – 2004 – 2003 – S3 S4 2004 – – 2004 W2 – W2 – – – 19.6 – 29.3 – – – – – 168 17 – 170 23.8 – 220 1 See separate entry 1 227.2 – Erfoud – 6 2950 L4 1 LL3.9 440 1 LL3.8 18 L4 1 – S2 S5 H4 S2 1 NAU3 W1 W2 CK4 Erfoud Erfoud W1 S2 Martian 26.8–32.4 22.2 S2 19.1–31.6 S2 W1 – 21 20.8 – W2 23.9 – – NAU1 19 NAU1 – 19.5 – – Some chondrules 20.5 – darkened shock 17 Erfoud – – – – Erfoud 21 See separate entry NAU1 See separate entry Erfoud 21.4 Erfoud Erfoud NAU1 Erfoud 28 24.8 3.7 NAU6 NAU1 38 NAU5 NAU1 NWA 2307 NWA 2350NWA 2351NWA – 2352 NWA – – 2003 2357NWA 2358NWA – – – 2359 NWA – 2360NWA – – 2002 2361NWA – 2002 2362 NWA – 2363NWA 2364NWA – – 2365NWA – 2004 189 141.5 – 2366 NWA – 2002 1 1 – 2004 – – 2004 H4 L4 – 2004 – – 427 S1 – – S3 328 – 1 W1 – W2–3 1 – 24.6–25.9 16.6 – L4 56 L4 263 22.3 1 120 1 18.6 1493 S5 Partly melted S5 LL6 258 1 18 L5 W1 – W1 Erfoud 1 23.8 L5 CV3 S3–4 24.8 S4 W4 LL6 14.2 S2 28.6 S3–5 21.7 W2 NAU2 22.1 W1 S3 W4 – 23.7 25.7 Shock darkened 36.1–48.4 W2 23.2 Shock darkened Erfoud 30.9 21.4 – Erfoud Shock darkened 21.3 20.3 Prato3 Shock darkened 22 Erfoud 25 Allende-like matrix 20.2 Shock darkened Erfoud NAU1 Erfoud NAU1 Erfoud 13 – 24.2 21.5 NAU1 NAU1 22.1 NAU1 NAU1 Erfoud 28 NAU1 Table 7. Meteorites from Africa Table A246 S. S. Russell et al. Type (g) Info Erfoud 20.1 NAU1 ErfoudDortmund 3.6 NAU1 20 Mün7 Erfoud 21Erfoud NAU1 Erfoud 21 NAU4 22.3 NAU4 Place purchased Erfoud 21.1 NAU5 Hamburg 20 Mün7 Stuttgart 20 Mün7 Erfoud 21 NAU1 ; br, cv; br, Hamburg 6 Mün7 a 40 5.2 in ol in olivine avg in olivine Wo 3 3 3 O O O 2 10.9 2 2 Fs = 0.09 wt% = 0.06–0.10 components plectic pockets and shock veins lized shock melt partly S6 darkening = 0.05–0.34 wt% Fs (mol%) Comment ± 1.7 19.5 ± 3 br sv, Stuttgart 36 Mün7 Fa (mol%) – – – – See separate entry Erfoud 55 La1 subclass HL Continued. Weight (g) Pieces Class Shock WG Longitude (W) Latitude (N) (uncertain locations; numbered). Date found (mm/dd/yyyy) Possible or origin pseudonym – 2004 – – 123 1 Ure – –– 1.2–12.3 – 2002 Pigeonite – – 136 1 Achondrite – – – – See separate entry Erfoud 20.2 NAU1 b b NWA 2399NWA 2400 NWA – 2429NWA 2004 2431NWA – – 2433NWA 2434NWA – – 2443NWA – 2004 – 2004 2446NWA – – 2004 2004 – 11/2003 – 12/2003 – – 280 – – – – 1 – – – L4 206 – 36 1 24 S3–5 1 230 441 LL4 W2 1 1 1 CO3.3 32 23.9 L3.9 S2 1 H3–5 Dio S2 W2 20.6 R3 W2 S2 S1 – 24.6 37.2–41.4 W2 W1–2 Shock darkened – 17 ± 0.6 S2 23.4–25.6 – Erfoud 20.8 – 13.5 ± 4 – – Cr – br; minor type 3 28 ± 17 20.4 NAU1 – 10 ± 4.5 – Peak: ~Fa Erfoud See separate entry Erfoud Erfoud 21.4 NAU1 27.6 5.3 NAU1 NAU1 NWA 2427NWA 2428NWA Morocco – 03/15/2004 – 2004 – – 111.5 – 2 H3 1650 1 S1 Iron, IAB W1 20.8 – – Erfoud 20 Pol Name 2376 NWA 2377NWA 2378NWA – – 2379NWA 2380NWA – 2381NWA – 2004 2382NWA – 2004 2383NWA – 2384NWA – 2004 2385NWA – – 2004 – – 2004 2004 – 2004 – – – 2004 – 2004 – – – – – – 327 3141 – – – 1 1 – 68 4526 – L3.7 H3.5 132 1 1 298 3 58 S2 S2 How 418 1 LL5 410 1 LL W2 W2 1 L4 – 1 S2 4.2–22.6 2–24.6 LL5 LL4 – W1 – L3.8 – S2 – 29.9 S3 – S3 W1 – S1 W4 Cr W2 24.1 – – W2 28.9 24.1 27 3.8–24.8 – 20.8 – 24 – – 22.8 See separate entry – Erfoud Erfoud – Metal-silicate sym- See separate entry – Erfoud 21.7 Erfoud 13.6 NAU1 NAU7 Erfoud 21 20.7 Erfoud NAU1 Erfoud NAU7 23 11.7 NAU1 21.4 NAU1 NAU1 NWA 2386NWA 2388NWA – 2389NWA – – 2390NWA 2004 – 2391 2004NWA 2392 2003NWA – 2393NWA – – 2394NWA – 2004 – 2395NWA – – 2396NWA – 2003 2397NWA – – 2004 2398NWA – – 2004 – – – 2004 – 2004 – 2004 – 440 – 2004 – 2004 – 81 1 156 – – – – 1 – 1 – CK4 231 – – CK6 – 178 LL5 1 – 602 – – 828 1 – L4 277 1 S3–4 – 423 1 L4 W2 865 1 – L4 323 1 25.6 – S2–6 L4 718 1 L4 W2 – 1 S3–5 LL4 1 S3 15.4–18.9 W1 LL4 22.8 S4–5 L4 S3–6 24.4 – W1 11.0–15.3 LL3.5 W2 S2 W2 S2 Contains recrystal- – 23.4 23.5 Localized melt W2 S1 S3–5 24.1 W2 See separate entry 20.2 W1 28.2 Erfoud W2 See separate entry 29 23.4 20.5 23.2 Erfoud 21 Shock darkened 8.1–35.3 23.6 22 Shock darkened Shock darkened Erfoud – 23.2 19.9 16.2 Shock melt br NAU6 Erfoud Erfoud – NAU6 21.5 – Shock darkened Erfoud Cr NAU1 27.9 26.3 Erfoud NAU1 NAU1 22.7 Erfoud NAU1 23.1 Erfoud NAU1 20.1 NAU1 20.4 NAU1 NWA 2447NWA – 2448NWA 2449NWA – 2451NWA – 2452NWA – 12/2003 – 2453NWA 04/2004 – 04/2004 – 04/2004 – 04/2004 – – 04/2004 – – – – – – – 132 1545 – 1 284 6370 1 L5–6 176 1 1 L6 2280 1 LL6 S2 24 L6 L6 W2–3 S5 L3-6 24.5 S2 S3 W2 W2 S3 S3 27.5 W3 20 28.5 W2 25 W1–2 25.5 23 22 ringw.; cv, br, 24 20 sv 19.5 br sv, sv strong shock sv, Stuttgart Stuttgart Stuttgart 26 20 Mün7 Mün7 37 Mün7 Table 7. Meteorites from Africa Table Meteoritical Bulletin No. 89 A247 Type (g) Info Place purchased –8.1Be8 ––– 20.4 Be2 –2.8Be5 28.2 Be5 20.3 Be5 ; ; ; ; ; 5.9–7.1 5.8–18.7 5.4–17.5 5.9–16.5 5.2–17.3 a Wo Wo Wo Wo Wo 97 87.5–92.3 79.9–95.2 78.8–88.5 83.7–93.3 39.9–40.3 43.1–53.3 44.4–54.3 47.9–55.3 23.4–57.8 Fs Plag An Plag An Fs Plag An Plag An Plag An Fs Fs Fs –– – –– 20.5– Be5 13.8– Be5 – – 20.1 – Be5 20.9 Be5 15.3 Be5 1.9 15.8 12.3 11.1 11.5 Fs (mol%) Comment (1.2–34.2) (1.1–23.5) (1.9–23.5) (0.8–5.2) (1.3–28.6) ± 12 8.5 ± 7.4 br sv, Marie St. 19 Mün7 Fa (mol%) (0.5–30.2) (0.5–32.2) (0.6–25.2) (0.1–43.1) (0.4–34.2) Continued. Weight (g) Pieces Class Shock WG Longitude (W) Latitude (N) (uncertain locations; numbered). Date found (mm/dd/yyyy) 2003 –2004 –2004 – – 5009 – Several Euc – 280.2 – 1 – 11.9 Euc 1 – Euc High – Mod. – – – Pigeonite – 51–57.7 Pig:eonite 51.8–58.6 Pigeonite Possible or origin pseudonym Morocco 2004 Sa- Western hara –Morocco 2004 Sa- Western –hara Sa- Western –hara 37.8 – 2 Euc 1000 – 2 – Euc – High – 41.9–43.9 – Pigeonite 41.5–50.9 Pigeonite b b b b b Name 2454NWA – 2455NWA 2456NWA – 2459NWA – – 2460NWA 2461 06/2004NWA – 2462NWA – 06/2004 2466NWA – 06/2004 – 2467NWA 06/2004 – 2474NWA – – 06/2004 2475NWA – – 06/2004 – – 2476NWA – 06/2004 2477NWA – – 06/2004 – 2479 NWA – – 06/2004 – – – 06/2004 – 06/2004 – 222 – 06/2004 – – 06/2004 – 38 1 – – 166 166 – – 1 – H5/6 – 100 1 1 – 108 LL4–5 – 114 1 LL6 S3 LL3–5 – 446 1 1 S2 65 LL6 W1 1 S2 62 LL3 S5 116 W3 18 1 L6 110 W1–2 1 H3–6 S3 W2 176 21 1 27.5 S2 E6 1 29 W2–3 H4 1 S1 S1 L5 29.5 15.5 W1–2 H4/5 26.5 ± 2.5 23 W2–3 W1 H5 24.5 S2 cv sv, 12.5 ± 7 23.5 19 ± 4.5 S3 S4 24 br cv, W2 sv, – W3 S3 W1 W2 13 ± 5.5 sv 20 18 – 24 br sv, cv, W3 18 br sv, Marie St. Marie St. 17.5 cv 22 15.5 Marie St. Marie St. 20 0.3 15.5 8 Mün7 Marie St. 15.5 Marie St. sv Mün7 20 20 – sv sv 20 38 – Mün7 Marie St. Mün7 Mün7 Mün7 25 Marie St. Mün7 Marie St. Marie St. Marie St. Marie St. 10 20 10 20 Mün7 20 Mün7 Mün7 Mün7 Mün7 NWA 2480NWA 2481 NWA Morocco 2004 2482 NWA 2483 NWA – 2484 NWA – 2485NWA 2486NWA Morocco 2487NWA Morocco 2003 Morocco 2488NWA 2003 4.1 2489NWA 2004 Morocco 2490NWA Morocco 1 2003 – Morocco 2491NWA 2004 – How 2492NWA 2004 Morocco – 2493NWA Morocco – 2004 2494 –NWA Morocco – 2004 2495 – –NWA Morocco – 2004 2496 –NWA Morocco 2004 Morocco – – 2497 –NWA 2004 – – 61.7 2004 Morocco – 109 2498NWA – – 1 127 2499NWA 2004 Morocco – – 18000 2500 1NWA Morocco – – 2004 1 Morocco – H5 – Several 2004 14.1 – L5 H5 2004 – 60 – H3 – 2 – 651 – S4 1 162.3 – L6 S6 S4 – 288.2 1 – W3 1 S2 See separate entry 490 H3 1 – W1 W1 149 – 17.7 – H6 W2 LL6 132 1 S2 17.7 22.6 – L6 1 15.9 S2 166 1 W1 H6 15.8 S2 S4 6000 L6 W2 1 23.7 15.1 19 H3 S6 1.15 82 W3 W1 1 13 Be8 72 – S3/4 CO3 W1 18 29.7 2 S2 Partly melted rock W2/3 H6 19.6 – 1 S2 23.8 – 17.3 W3 S2 LL6 W2/3 H3 23.8 – 23.9 12.2 S2 15.9 W1 20.6 15.4 S4 – 20.7 W3 – 22.4 S2 – – W3 20 18.1 Be2 Partly melted rock – W3 29.7 – – 10.3 17.7 – 16.1 Be7 23.4 24.1 – – Be7 20.1 – – Be5 sv 3.8 br, Be5 – 21.9 21.9 Be5 25.5 Be5 – – Be5 21.7 Be5 20 18.8 Be5 Be5 Table 7. Meteorites from Africa Table A248 S. S. Russell et al. Type (g) Info Erfoud 22.5 Pa17 ErfoudErfoud 15.8Erfoud Pa17 9.6 Pa17 18.5 Pa17 Place purchased – 20.6 Be5 Erfoud 20.9 Pa17 HamburgRissani 7 25.7 Mün8 Erfoud Mün9 11 Mün10 21.5–48.7 ; a Wo 4.4 90 ± 2 90 Wo 7.7–19.9 51.6 =3.13 =3.23 = 4.35 Erfoud 3.3 Pa17 –Fs – 33.9 Be5 –br; partly melted – – 22.3 20.4 Be5 Be5 and opaques, χ Fs χ See separate entry, See separate entry, est. subtype 3.6/3.7 Zoned ol, px; melt pockets, est. sub- type 3.7 nodules, est. subtype 3.9 χ contains type 6 fragments ol, px between clasts 5.7 3.5–27.7 2.4–33.2 0–0.5 About 10% metal Marie St. 6 Mün7 11.7 16.1 (1.9–25.2) Fs (mol%) Comment (1.8–25.2) (0.8–16) (18.2±8.9) (14.3±6.1) Fa (mol%) (0.4–48.8) (1.1–23) (25.8 ± 7.7) (18.2 ± 7.3) (0.6–38.2) W3/4 7.5–42.3 1.1–24.9 br; Augite Continued. 1 Dio2 Euc1 S3 Ure W3 – – W2 S4 – W2 26.5 22.6 ± 0.2 19.1 56.4 Rare plagioclase Pigeonite 1 H4 19.1 ± 0.3 16.8 ± 0.15 – Erfoud 8.3 Pa17 1 CK4 S3 W2 31.3 ± 0.4 27.0 ± 1.1 See separate entry Erfoud 9.4 Pa17 1 LL31 S4/S5 W4 LL3 0.9–32.3 S2 W3 28.1 ± 0.2 23.5±1.2 opaque Well-sep. 11 H/L3 S3/S4 W2 0.7–37.9 Weight (g) Pieces Class Shock WG 2 4 4 2 7 3 3 2 Longitude (W) Latitude (N) (uncertain locations; numbered). Date found (mm/dd/yyyy) Possible or origin pseudonym –– 01/09/2004– – 01/09/2004 – – 01/09/2004 – – 217.6 – 295.7 17.6 b b b Name 2501NWA Morocco 2502NWA 2004 Morocco 2503NWA Morocco 2004 2504NWA 2004 – Morocco 2004 – – – – – – 1165 – 1 590 400 H3 4 3 382 CV3 S2 R3–6 5 W2 S2/3 H3–4 S3 17.1 W3 7.5 S6 W1 19.8 NWA 2505NWA 2506NWA Morocco 2507NWA Morocco 2004 2508NWA Morocco 2004 2509NWA Morocco 2004 2510NWA Morocco 2004 2511NWA Morocco – 2004 2512NWA Morocco – 2004 2514NWA Morocco – 2004 2515 NWA – – 2004 – – – 2516 NWA – – – – – – – – 390 2518NWA – 395 – – 1 28 1 – 14.7 4000 1 L5 1 755 L6 1 124 01/09/2004 – H4 250 1 CK4/5 1 – H6 S4 1 S4 L3–6 S2 W2 L3–6 S6 W2 – CO3 S2 W2 23.3 6.6 S2 W0/1 23.6 S2/3 32.4 17.3 W0/1 1 W3 S2 W3 17.9 19.7 15.6–28 H4 W1 30.9 19.8 0.6–30 15.1 – 15.8 0.7–45.2 – 6–23.7 – S1 1.1–24.4 Partly melted br 1.0–5.2 – – – W4 – – 16.8 – – – 18.3 – – – 6.7 – Be5 – 23.6 21.6 Be5 20.7 Be5 20.2 22.5 3 Be5 Be5 20.1 Be5 Be5 Be5 – 3 Prato3 NWA 2519NWA – 01/09/2004 – – 44.4 NWA 2520NWA – 2521NWA – 2522NWA 01/09/2004 – 2526NWA 01/09/2004 – 2527NWA – 2528NWA – – 01/09/2004 2529NWA – – 2530NWA – – 2531NWA – – 06/26/2003 2532NWA – 2003 – – 2001 – P 01/2003 75.5 P 01/2003 – P 12/2003 – – 47.8 – P 12/2003 – – 135.1 – – – – – – 42.9 – 1 600 5273 52.7 E achond 57.1 1 1 210 1 – 1 33.3 2 Mes H5 LL(L)3 1 W2 L6 LL6 – – Dio S1 S3 S4 W1 – S4 W2 S2 W2 23.5 ± 0.5 19 W3 18.5 ± 8 W0/1 25.5 23 ± 1.5 30.5 – 15.5 ± 1 1 17 – 21 25 32 ± 2 cv sv 2 br; An Morocco Marie St. 20 62 Erfoud Mün7 Erfoud Hamburg Mün7 10.7 12.7 22 Mün8 Mün8 Mün8 NWA 2517 NWA 2533NWA – 2534NWA 2535NWA – 2536NWA – P 05/2002 – – P 12/2002 P 06/2002 P 01/2003 – – – – – – – 190 1 593 187 H 1 51.2 1 1 LL5–6 L5 – LL4–6 S3 W3 S3 W1 S4 20 29.5 W2–3 W2 30.5 24 24 17.5 25.5 19 melt br; Impact br sv, br; small vars in sv, sv Erfoud 22.2 Erfoud Mün10 22.1 Mün10 Table 7. Meteorites from Africa Table Meteoritical Bulletin No. 89 A249 Type (g) Info Place purchased Munich 7Munich Mün10 21.1 Mün10 Erfoud 21.3 NAU1 Erfoud 46 NAU1 Erfoud 4.2 Mün10 ; br 9.9 ; sv Munich 3 Mün10 ; a Wo ; sv, br; sv, Marie St. 21 Mün10 91 ± 1.5 91 ± 4 84 48–57 18.8 91.5 ± 91.5 2 imb Plag: An An 3darkening Munich 4.3 Mün10 rock 0–11 – Munich 4 Mün10 21.5 Fs (mol%) Comment (21–30) (eq. lith) Fa (mol%) (eq. lith) (0–41) Continued. 1 Martian – – – – See separate entry – – – Weight (g) Pieces Class Shock WG 7 Longitude (W) Latitude (N) (uncertain locations; numbered). Date found (mm/dd/yyyy) 2004 – – 100 1 Iron, IIICD – – – – See separate entry Erfoud 17 La1 Possible or origin pseudonym – 2004–– – 2004 2004 – – – – 241 – 1 Ure 244 600.2 1 1 – Dio Ure – – High 9.8–19.6 – – 16.8 3.8–21.4 28 – – 23.4 Pig: Fs Erfoud – 21.6 NAU1 Erfoud 22 NAU1 Africa b b b NWA 2625NWA 2626NWA – Algeria 2004 2634 NWA 2004 – – – – 31.0 305 1 Ure – – – – See separate entry Erfoud 22.2 NAU1 Name 2537NWA – 2538NWA – P 04/2003 2542NWA P 06/2003 – – 2543NWA – – – P 06/2003 – P 11/2003 – – 65.4 – 215 1 – 1 L6 Mes 20 S4 1 33.9 S2 W3 4 L3–6 W0/1 24.5 Euc – S2 20.5 W1 S2 26.5 ± 2 25 W2 partly S5 cv, sv, Stuttgart – 21 14.7 Mün10 – fragments of br, sv, Opx: Fs NWA 2539NWA 2540NWA – 2541NWA – – P 06/2003 P 06/2003 P 06/2002 – – – – – – 34 25.1 42.6 1 1 1 LL6 LL6 L5/6 S3 S3 S3 W3 W1 2627NWA W1 2629 NWA – 30.5 28.5 24 24.5 2004 23.5 20 sv br sv, – – – Marie St. Marie St. 5.4 Erfoud 6.9 68 Mün10 Mün10 1 9.3 Acapulcoite Mün10 – – – – See separate entry Erfoud 13.7 NAU1 NWA 2544NWA 2545NWA – – 2546NWA – 2547NWA P 11/2003 2548NWA – P 11/2003 2549NWA – – – P 11/2003 2550NWA – 2618NWA – P 11/2003 2619 –NWA – – P 11/2003 2620NWA – – P 11/2003 – 2621NWA – – 2622NWA – – P 11/2003 – 2623NWA – 2004 – – 2004 – 2624 NWA 15 – 2004 19.7 – 2004 1 – 185 2004 1 – – 2003 287 – 1 L(LL)3 L3–6 – – 28.8 1 – – 17 2635NWA S2 H5 1 – – 2639NWA – S2 14 – 2641 1NWA L3–5 W2 – H4 – 2644NWA – W0/1 1 26 ± 10 S4 – 152 2645NWA – 25.5 CV3 ox 220 2668 S2NWA – 2004 1304 2669 W1 1NWA Morocco Euc 2004 S1 S1 4639 17.5 ± 8.5 2670 1NWA W3 Morocco 2004 1 20.5 sv 2003 827 2671NWA Morocco 2004 L6 W1 W4 1 23.5 ± 10.5 2003 153 2672NWA Morocco – 2004 H4 S3 2003 2673 1NWA H4 Morocco – 18.5 28 ± 16 18.5 ± 9.5 2003 2674 1NWA L4 Morocco – 18 br sv, W2 – 2003 2675NWA Morocco S2 – – LL4 – 2003 2677NWA S2 Morocco – – L4 S2 – 2003 16.5 ± 1.5 Northwest W3 Munich – – S2 2004 – silicate sv, W3 Porous – S3–5 – W2 24.2 – – – W2 18.2 Munich W2 – 4200 S3–6 18.5 – – 3.1 W2 539 24.9 62 ± 3 28.2 – – 1 Mün10 20.6 97 – 165 25.3 Munich 23.1 216 3 16.4 Plag: An – 336 16.9 166 Mün10 ung Achond 1 – 1 – 20.9 66.8 23.5 1 – Mes 117 1 1 – 6.8 1 22 425 – How H6 – How 1 Mün10 – 45 – H4 EL6 1 – L4 92 3354 – 1 H4 Recrystallized melt – – S2 1 H6 1 – S3 – Erfoud H5 – S4 W3 Erfoud – H6 Erfoud L6 S2 W2 – – 18.6 Erfoud W2/3 S2 Erfoud – – 15.6–16.8 21.4 21.1–25.2 W3 – S2 20 W2/3 NAU1 S4 21.1 – S4 17–18.3 13.9–15.1 17 W1 17 9.1–17.2 16.2 20.8 NAU1 NAU1 See separate entry – – W3 W1 – NAU1 17.4 Erfoud NAU1 – 5.4–19.2 – 17.6 24.8 – – – 15 See separate entry 23.2 15.5 See separate entry Erfoud See separate entry 15.6 NAU1 21.5 Erfoud – See separate entry Erfoud – – – Erfoud 21.1 – – – – 18.8 NAU1 22 NAU1 21.3 23.6 NAU1 15.3 NAU1 Be5 – Be5 21 – 21.5 – – Be5 Be5 20.3 9.2 Be5 18.4 26.6 Be5 Be5 Be8 NWA 2738NWA – 2004 – – 370 1 How – – – – See separate entry Erfoud 30 NAU1 Table 7. Meteorites from Africa Table A250 S. S. Russell et al. Type (g) Info – 26.6 Vr3 Er-Rachida 7– Pa1 Tokyo 20.5 Pa20 20.5– Pa3 31.77 Pa20 Place purchased a = 0.9 wt% –stone Zagorastone 19.8 Ham1 pockets texture – – 21.3 Be5 0.9–29.8 Co in kamacite 20.4 ± 9.8 14.5 Fs (mol%) Comment (48.1) (2.5–21.3) 9 22.3 ± 0.9 small melted Many ± 0.5 26.5 ± 0.7 br Kem Kem 15 Ham1 ± 0.4± 0.2 21.8 ± 0.3± 0.2 Entirely crusted 16.9 ± 0.16 – 21.6 ± 0.5 Entirely crusted Er-Rachida 11.9 Pa1 ± 0.6 16.9 ± 0.8 br El Mahabas >20 Ham1 Fa (mol%) (48%) (62.4) (17.3–24.7) 2/3 18.0 ± 0.7 15.9 ± 0.4 – – 35.2 Pa20 Continued. Weight (g) Pieces Class Shock WG Longitude (W) Latitude (N) – – 15441 10 L4 S4 W2 21.8 ± 0.6 18.8 ± 0.5 Clear chondritic (uncertain locations; numbered). Date found (mm/dd/yyyy) 2004 – – 950 1 L3 S3 W3 0.6–36.3 2003 Possible or origin pseudonym Africa NWA 2808NWA 2809NWA Morocco Morocco 2003 2003 – – – – 2875 4850 1 1 H6 LL6 S3–4 S3 W0–1 19.0 ± 0.3 W2 16.7 ± 1.1 32.3 ± 1.3 4 24.1 ± 1.9 br Tisgui-Remz >20 TarfenNouss Ham1 >20 Ham1 NWA 2816NWA 2817NWA Morocco? 2818NWA Morocco? 2003 2819NWA Morocco? 2003 2820NWA Morocco 2003 Morocco 2003 – 2003 – – – – – – – – – 114 337 156 1 1 80 1 200 H4/5 Ure 1 1 H5 S2 How LL <3.5 – W3 S2 S2 S3 18.8 ± 0.2 – W4 W2 16.8 ± 0.1 W0 22.2 ± 0.3 19.8 ± 0.4 –14.2 ± 22.81 – 17.5 ± 0.3 – br 5 – – – – >20 – Ham1 >20 Ham1 Zagora >20 Ham1 16.2 Ham1 Name 2739NWA Algeria 2740NWA 2741NWA – 2807 2002/2003NWA – Northwest – – 2810NWA – Morocco 2811NWA – 2813NWA Morocco 2003 2814NWA Morocco 2003 Morocco – 2003 – 2003 – 824 – – 4 – – – – How – – 53822 – 1350 – 2073 3 1 950 1 – L5 194 LL5 76 1 H5 – 1 S1 1 L4–5 S1 L6 S3 W0 LL6 W0 S3/4 – W1–2 20.9 19.1 W1–2 29 S3 26.8 ± 0.3 S3 separate entry See W2 22.5 ± 0.1 24.5 W0 – 24.6 ± 0.3 br; cv 23.6 31.1 – – – 35 El Mahabas sv br, NAU1 >20 – Ham1 – Kem >20 30 Ham1 20.8 Prato3 Prato3 NWA 2872NWA 2873NWA Morocco 2874NWA – 2000 2875NWA Morocco Morocco 2876NWA 12/2004 2877NWA 12/2004 Morocco 2002 – – 2878NWA 12/2004 – 2879NWA – – 2880NWA – – – 2881 –NWA – – 12/2003 – – 2882NWA 2002 2883NWA – – – 2004 – 2884NWA Morocco 2004 859 – 1800 2004 2885NWA 12/2004 – 2886 1NWA – – 32 2004 6 – 3043NWA – – 36 3044 –NWA 51.7 Morocco 1 Ure 2001, 2002, – – 3045NWA LL6–3 Morocco 1 1 – 2003 3046NWA Morocco 19200 01/02/2003 – L6 – 2003 Morocco – 02/2003 S4 3047NWA S3 – 2003 H5 – How 1 3048NWA 2003 Morocco W1/2 – 3049 –NWA W2 120 Morocco – S2 2380 27.0 ± 0.3 2003 3050 –NWA L/LL6 Morocco – 23.7 ± 0.2 S3 2003 3051 –NWA Morocco 1 145 63 W1 1 2003 3052 –NWA Morocco – 7.3–22.8 96 S3 – 19.7 2003 W2 3053NWA Erfoud – W1 25.6 6 1 1 L4 – 2003 3054NWA Erfoud – L4/5 47 1 18.9 W2 – 11480 Zagorra – 2002 – – L5 H6 25.4 1 2002 Several – 1440 – LL5 2003 S3 S4 H6 754 – – 58 H6 2400 1 – – W2 W3 S3 S2 1 – Er-Rachida S4 22.3 – Many 80 1 – S2 – 24.5 ± 0.4 23.8 ± 2.1 L6 W4 W3 H6 LL6 W3 20.37 77.6 S2 – – 1 W 20.6 ± 0.3 21.3 ± 0.4 H4 Pa1 See separate entry 63 19.7 ± 0.2 25.3 ± 0.2 – 1 25.8 ± 0. – 8 7 21 W4 – 315 S4 L3 S2 17.4 ± 0.4 22.4 ± 1.5 1 S4 1788 19.8 ± 0.3 H6 1 – – S2 1 W1 W1 859 W0 1 H6 27 17.4 ± 0.3 S3 W2 24.1 L6 2613 70 31.6 17.9 Pa4 – L6 S4 1 L5/6 7.4 18.2 W1 1 Munich – 1 S2 Pa2 W2 L6 S6 22.8 20.4 26.1 16.4 S4 S6 Munich Er-Rachida H4/5 H4–6 W2 18.8 20.3 16.4 W2 W3 W1 19.3 20.1 Pa3 – – Munich – S3 S2 25.6 21.5 S3 14 Pa1 25.7 25.4 – 16.6 Pa2 W3 W1 W0 Pa3 17.2 10 25.7 19.4 21.8 17.6 – 21.7 22.6 Pa3 – – – – rw sv, – Partly melted rock 21.9 17.4 15.6 – – – br – – 25.2 27.5 20.1 – – Be5 Pa20 13 Be5 21.3 – Be5 Be5 20 – – – 5.4 12.8 Be5 Be5 Be5 33 Be5 14.6 21.8 5.8 Be2 Be2 Be2 Table 7. Meteorites from Africa Table Meteoritical Bulletin No. 89 A251 Type (g) Info Place purchased –21Be2 a 1.4 ––––6.4Be2 –– –––3.5Be2 22.1 Be7 20 – Be7 20 Be2 ––2.3Be2 sv – 51.5sv Be6 – 20 Be5 9.8 16 12 19.3 16.2 Fs (mol%) Comment (8.6–17.1) (3.3–17.3) (9.7–18.2) (4.9–21.9) (9.8–17.1) (0.8–19.5) (13.5–23) (2–26) Fa (mol%) (0.8–27.8) (3.4–21.9) (6.2–23) (10.6–32.4) (0.8–26.8) – – – – See separate entry Rissani 20.2 NAU achondrite Continued. 1 EL6 – – – – See separate entry Rissani 13.8 NAU Weight (g) Pieces Class Shock WG 5 Longitude (W) Latitude (N) (uncertain locations; numbered). Date found (mm/dd/yyyy) Possible or origin pseudonym Name 3057NWA Erfoud 3058NWA 3059NWA Tagounite 3060NWA 2003 Tagounite 2002 3061NWA Tagounite 2002 3062NWA Tagounite 2002 3063NWA Tagounite 2002 – 3064NWA Tagounite – 2002 Tagounite 3065NWA – 2002 3067NWA 2002 Tagounite – – Tagounite – 2002 – – 2002 – – – – – – – 138 – – 750 – 203.2 1 – 147.2 1 1 489.8 – 1 L6 88.9 2 L6 H4 813 1074 1 L6 H6 2 114.3 1 S6 140 S4 L6 1 S2 LL6 LL6 W0 S3 5 W1 S4 W3 L6 21.8 W2 24.9 S3 18.2 S4 H4 W0 S4 25.4 W1 19.5 W1/2 S6 W2 18.8 29.6 24.8 21.3 16.2 S2 31.2 W3 21.8 Partly melted rock 17.2 W1 25.3 – – – 25.1 21.1 17.7 – 25.9 – br 21.5 – – 14.4 26.8 Be2 rw sv, – – – – – – – – 25.6 24.1 Be7 23.2 Be7 27.8 Be7 22.5 Be7 20.8 Be7 25 23.2 Be7 Be7 Be7 NWA 3068NWA Tagounite 3069NWA 2002 3070NWA Erfoud 3071NWA Erfoud Erfoud 2002 3072NWA 2002 – Erfoud 3073 2002NWA Erfoud 3076 2002NWA – – – Erfoud 2002 – – 2002 – – – 147.8 – 1 – – 1200 – L3 27 1 – 30 1 150 L5/6 1 S3 4 LL5 15 H3 W1/2 S2 80 11.8 1 H4 S2 W2 1 H4 S2 25.2 W2 S2 H6/7 W1 28.6 W1 S2 16.8 21.6 S2 18.4 W3 24.3 W0 – 19.3 18.3 13.1 – 14.4 16.1 – Wo – 25 Be2 5.6 Be2 NWA 3101NWA 3102NWA – – 2003 2003 – – – – 151.7 68.1 1 H6 S2 W1 18.8 16.7 – Rissani 20.2 NAU NWA 3077NWA Morocco 3079NWA 3080NWA 2003 Morocco 3084NWA Morocco 2003 3085NWA Morocco 2003 3086NWA Morocco 2002/2003 3087 –NWA Morocco 2002/2003 Morocco 3088 –NWA 2002/2003 – 3089 –NWA 2002/2003 Morocco – – 3090NWA Morocco – 2002/2003 3091NWA Morocco – – – 2002/2003 3092NWA Morocco – – 2002/2003 3093 –NWA Morocco – 2002/2003 3094 –NWA Morocco – 11.2 2002/2003 3095 –NWA Morocco 2003 3096 –NWA Morocco – 314 1 434 2003 3097 –NWA Morocco – 139.3 300 2003 3098NWA Morocco – 1 354 1 1 Ure 2003 3099NWA Morocco – 518 1 – 2003 Morocco – 1 3100 – H4NWA 2003 H5 L6 171 1 – 2003 Morocco H5 – 227 – – L6 221 1 2003 – – L3/4 338 1 S2 S4 W1 – S6 – 276 3103 1NWA S2 – L6 – 1 18.3 W3 – S5 W2 L5 – W0 S4 1 – W4 H4 – 17.5 20000 18.9 94 21.9 W2 L5 – W2 18.2 S4 L6 Many 470 S4 23.9 1 2003 – 22.3 232 L6 S3 W3 15.5 256 1 16.1 S4 19.1 W2 CO3 1 15.9 24 78.7 S4 W3 179 1 23.9 20.3 – W2 CV3 1 S6 – 17.1 – Partly melted rock W2 L6 136 S2 1 – 25.2 H6 – W1 22.4 – R5 S1 20.4 – 1 20.3 W1 L/LL3 23.2 15.6 S6 W2 22.3 S2 0.7–52.6 Primitive – S3/4 S4 19.4 sv W1 – 0.2–43 – – 20 W3 W3 19.6 1.1–47.3 – 21.3 – W1 74 – 17.9 – Be6 – 38.6 20.5 1–1.5 1 Partly melted rock 18.3 – 40 – 28.1 – – LL3 16.1 38.9 – Be6 – Be6 32.4 Be6 – Partly melted rock – Be6 – – S2 – – 31.7 30 36.8 W3 Be5 – 28.6 Be6 Be6 7.5–42.4 26.3 Be6 22 21.7 Be6 20 Be6 – – Be5 Be5 – 22.8 Be5 – 23 16 Be5 Be5 Rissani 22.1 NAU Table 7. Meteorites from Africa Table A252 S. S. Russell et al. Type (g) Info Erfoud 8.6 NAU Erfoud 3.8 NAU Place purchased Erfoud 6.5 NAU Erfoud 21.1 NAU Erfoud– 20.1– NAU 20.1 NAU – 21.7 UWS ––20UWS –20UWS1 20.6 UWS – 20.7 UWS 11.1 UWS1 ; ; ; 1.3 8.2– 3.3 9.1 Wo 16.1–6.5 43.5–44.4 44.9–44.3 44.1–43.8 0.1–0.2 0.3–0.4 Or a Wo Wo Or Or 62.7 Wo Wo Wo Wo 86–70 17.8 17.9 90.8 89.1–90.7 88.7–89.6 56.3–63.5 26.4–28.7 25.1–27.1 25.9–26.2 2.0 (9.9% Ni) and troi- lite Fs An Augite Fs Fs Augite Fs Fs Plus 21.4 g at UCLA pts at UWS 310; plus NWA 3.7 g at NAU Fs (mol%) Comment Fa (mol%) – – – – See separate entry; achondrite Continued. Weight (g) Pieces Class Shock WG Longitude (W) Latitude (N) (uncertain locations; numbered). Date found (mm/dd/yyyy) 2004 – – 95 1 Lunar – – – – See separate entry – – – Possible or origin pseudonym Morocco 2003Morocco 2003 – – – – 51 1 32Morocco Ure 2003 1 Ure – – – S2Morocco – 2002 – 21.1–2.3 23.3–7.6 16.9 – 131Morocco – Contains metal 1 2003Africa –Morocco Euc Pig: Fs 2004Morocco – 132.1 – 2004MoroccoMorocco – 1 – 2004 – 08/2004Morocco Euc – – 08/2004 – – – – – 45.8 – 1 – – 931 – 56.4–59.3 – Plag An Ure 1 132 – 249 750 Euc 1 – 1 1 44 Euc – – – 1 Euc Ure 23.2–8.1 – – Euc Pigeonite – – 18.7 – – – – – Pts at UWS – – 22.2–13.8 – 61.6–2.0 – An – – 62.7 63.1–64.7 An Cpx: Pig: Fs 20.1 60–62.2 NAU Cpx: b b b b b b b b b b NWA 3109 NWA NWA 3136NWA Northwest Name 3104NWA – 3105NWA 3106NWA Morocco 3107NWA – 2001 3108 NWA – 2003 2003 3110NWA – 2003 Morocco 3111NWA – 3112NWA Morocco 2003 3113NWA Morocco – – 2003 3114NWA Morocco – – 2003 3115NWA Morocco 2003 3116NWA Morocco – – 2003 3117NWA Morocco – – 2003 Morocco ~10000 – 89.2 2003 – Many – 2003 1 – – CV3 – 130 – – CR2 66.85 – – 1 – S2 173 1 – – – W2 356 Diog 1 H6 – 143 236 1.3–38.7 1 – LL3.9 1 – 70 1 – S2 34.7 LL3.9 – S2 27 1 LL3 – 1 234 W2 H3 S1 W1 1 – L3.8 3 18.9 H4 – S2 27.1–30.3 W1 CK5 – S2 How 21.4–24.7 W2 26.0–30.6 S2 – S2 17 W2 27.4 21.2–23.6 S3 W1 – – See separate entry 16.2–18.8 W2 – Rissani 19.2–25.6 3137 RissaniNWA – – 18.2 14.8–15.4 – 24 17.3–22.1 See separate entry – – 21 – 12.35 Rissani Zagora – NAU 16.3 NAU – Erfoud 20.6 20.4 Rissani – – NAU NAU – Erfoud 20.1 Erfoud 13.4 NAU See separate entry Zagora NAU See separate entry 20.1 Erfoud 14 NAU Zagora 20.5 NAU NAU 5.4 NAU 6.94 NAU NWA 3118NWA 3119NWA Morocco 3120NWA Morocco 2003 3121NWA Morocco 2003 3122 NWA Morocco 2003 2003 – – – – – – – – 5895 1073 Many 68 CV3 1 164 1 1 LL4 – L3 LL6 – S2 W1 S2 S3 – 28.4 W1 W1 22.5 28 – 23.6 19.1 23.3 – See separate entry Erfoud – – 20.3 Erfoud NAU Erfoud Erfoud 20.8 NAU 14.2 20.1 NAU NAU NWA 3123NWA 3124NWA Morocco 3125NWA Morocco 2003 3126NWA Morocco 2003 3127NWA Morocco 2003 3128NWA Morocco 2001 3129 NWA Morocco – 2001 – 2001 3133NWA – Morocco – – NWA 3134 – – 2004 Morocco – – 3135 NWA – 2004 – – – 48.1 566 1 577 – 173 1 3138 NWA – 487 1 H6 3140 532NWA 1 – L5 3141 NWA 1 LL5 1 LL3.7 3142 NWA S2 4193 LL3.1 S1 LL3.8 S2 Several W1 S4 970 Primitive S2 W2 25.1 W2 S2 W4 1 24.4 W3 30.5 24.6–34.5 W1 EL6 – 21.3 23.4–33 – 20.3 25.6 – 18.5–24 – – – – – – W0 – See separate entry – Erfoud Erfoud Erfoud Zagora Erfoud – 21.5 25.1 NAU 20.3 21 20.8 22.1 Possibly paired with NAU NAU NAU NAU NAU Table 7. Meteorites from Africa Table Meteoritical Bulletin No. 89 A253 , olivin rim: Type (g) Info , only few olivines, 22.19 ± 0.33 94.5 ± 3 Wo (mol%) Type Info pact melt br with H clasts; Ol in Place purchased Rissani 20.5 UWS –11.3Be2 – 22.7 UWS1 t, 1.2 cm in size; native copper areas; ; , Fs (mol%) 0.4 rst one was NWA 757 (Bischoff A. 2002, 757 (Bischoff rst one was NWA 21–29 7–12 Or ); (5) olivine core: Fa 42 Wo ; Wo a Wo k veins; Notes: (1) An 89.2–90 89.9 30 22–48 43–59 Fa (mol%) entry Aug Fs Aug Pig Fs cpx: Fs Fs (mol%) Comment rance as NWA 722 (L clasts rance as NWA ly few unequilibrated components; (4) im ngw – ringwoodite, sv shoc chondrite having ringwoodite. The fi ww.meteoriticalsociety.org). oned; estimated subtype 3.8; (7) melted pocke Fa (mol%) 8.9 1 H4/5 S1 W2 18.7 ± 0.2 16.4 ± 0.2 1.3 ± 0.3 1.76 Bart1 16 kg 1 H5 – W1 18.7 18 3.4 59.4 Vr11 20.02 kg 1 H4 S1 W1 20 5–24 0.2–7.2 2034 Vr9 14.3 1 H5 S1 W3 19 16.5 1.3 22 Vr8 45 1 H6 S4 W3 19.1 17.9 1.3 10.75 Vr7 207 1 L5 S3 W1 25.4 22.2 1.5 24.1 Vr10 200 1 H5 S4 W2 18.95 16.43 1.43 22.1 Prato5 120 1 L5 S3 W1 23 20 – 80.8 Sn5 2167 1 L6 S3 W2 24.3 20.8 – 165 Vr12 Mass (g) Pieces Class Shock WG ; May be paired with NWA 3137. ; May be paired with NWA melt; macroscopical appea ′ ′ ′ may be the second LL – – – – See separate entry Erfoud 28.6 UWS ′ ′ ′ ′′ ′′ 42–44 20 ′ ′ 01 ′ Wo Bulletin Web site (http://w Bulletin Web 41°30.276 81°58 21°32.99 79°40.877 7º12 36°58.68 44°51.57 11°21 55°14.098 Longitude (E) 25–27 ′ ′ ′ Dio – – – – br; see separate achondrite ′ ′ ′ ′′ ′′ y be paired; (3) sv, br, fragments of imb; on br, y be paired; (3) sv, 42 30 ′ ′ ′ Continued. melted veins; in type 3 part, opx is z s in metal droplets monomict breccia, pbr – polymict ri , ringw; partly S6. This Latitude (N) ailable on the Meteoritical at the edge; (9) Aug Fs 3 Weight (g) Pieces Class Shock WG O 2 Date found (mm/dd/yyyy) Longitude (W) , 0.3 wt% Cr Italy 07/152003 44°29 15–20 ; (6) br, small angular clasts separated by ; (6) br, Latitude (N) on of these meteorites is av 6.17 veins, imbr – impact melt breccia, mbr (uncertain locations; numbered). Wo Conference, abstract #1264). These two samples ma 75.12 metal abundance in studied thin section); (2) sv Tarnobrzeg Poland 03/2000 50°54.20 Altai Region Russia 09/21/2003 52°25.443 Romagna En melt: 17.33 (5.17%); shock blackening; sulfide bleb Date found (mm/dd/yyyy) 2004 – – 138 1 Euc – – – 62.4–63.1 Plag An 18.72 of zoned olivines, Fa zoned olivines, of tokrzyskie Í wi Prov. å Dist Argentera MtsArgentera Cuneo Italy 08/1995 44º11 Possible or origin pseudonym MoroccoNorthwest 2005Africa –Morocco 2002 – – 290 – 1 Euc 48.6 1 – Euc – – – – 60.5–61 – 9 – Tagounite Plag An 20.3 UWS b b b melt: 18.64 (2.01%), opx in 31st Lunar and Planetary Science br; or anom. achondrite (rel. low (8) melted pocket made up 19.10 ± pyroxene: Fs 2,45; NWA 3146NWA 3147 NWA Morocco 2004 – – 304 Several R4 – – – – See separate entry Erfoud 20 UWS NWA 3148 NWA Name 3143NWA Morocco 3145NWA 08/2004 Morocco 2004 – 3149NWA – Morocco 3171NWA – 3172NWA Algeria 08/2004 3175 NWA – – 2004 – 2335 – 1 – – 678 – 1 – 2594 Primitive 1 – 506 How 1 21029 – Martian 1 – – L – – – S6 – W0 24.1 ± 0.5 – separate entry See – – See separate entry – Impact br 20 UWS1 – 22 UWS1 100 UCLA A separate entry providing a fuller descrpti Zubkovsky – Region Rostov Russia 08/2003 49°47.350 Podgrodzie Zerkaly – Altai Region Russia 1956 52°08 Markovka (b) Klyuchevskoy Lago Valscura Koltsovo Kaluga District – Russia 07/2004 54°45.03 Issa Penza District – Russia 2002 53°52.05 Castenaso – Emilian- Name District State Country Beyneu Beyneuskiy Mangistauskiy Kazakhstan 10/19/2001 45°27.798 Abbreviations: br – breccia, cv calcite Table 7. Meteorites from Africa Table a b Table 8. Eurasian ordinary chondrite finds. Table A254 S. S. Russell et al. c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name LAP 02234LAP 02235 LL6LAP 02236 L5LAP 02240 LL5LAP 02241 H-imp 24.18LAP 02242 LL5LAP 02243 A/B 31.11 H5 40.04LAP 02244 28.16 B/C H5LAP 02245 A/B C 106 LL5LAP 02246 LL5LAP 02247 LL5 6.86 A/BELAP 02248 11.67 – 106.46 H5 BLAP 02249 108.35 23 B/C LL5 A/BLAP 02250 – 127.4 LL4 A/BLAP 02251 18 – LL5LAP 02252 20 A/B 25.33 – L4 68.02LAP 02253 – B/C H6 16 20.74LAP 02254 A/B – LL5 – 94.3 – –LAP 02255 A/B – – H5 – – 119.03LAP 02256 – – A/B LL5 –LAP 02257 C 20.76 – L5 – – 78.66LAP 02258 – – – C – LL5 – 114.6LAP 02259 – A/B – LL5 – 94.8LAP 02260 – – A/B LL5 – 162.77LAP 02261 – – 132.33 A/B LL5 – –LAP 02262 – – A – – – LL5 A/B 23 32.88LAP 02263 – – – LL5 54.55LAP 02264 A/B – 144.88 – LL5 – – –LAP 02265 A 19 – 118.3 19 L5 A/BLAP 02266 – – LL5 – – 45.35LAP 02267 B – – LL4 – – 92.22 –LAP 02268 16 A/B – – H6LAP 02269 – A/B – 60.33 L5 – – 52.13LAP 02270 – 141.88 B/C – CM2 –LAP 02271 – – – B – LL6 – A – LAP 02272 39.85 – – LL5 –LAP 02273 – – 17.81 C 24.24 LL6LAP 02274 – – – – – – B/C LL5 14.75 BLAP 02275 – – – H6 –LAP 02276 A/B – 9.17 – LL5 – 39.59LAP 02277 – – – – A LL5 – 25.25LAP 02278 B/C – – CM1 –LAP 02279 A – 26.16 – – H5 0–27 38.18 –LAP 02280 – – – C L5 – – 44.16LAP 02281 B – H5 – LAP 02282 – 7.76 B – LL5 – – 30 – – A – LL5 3.44 – – – 2269 5.32 C – – 17.18 25 – – 18.78 – C C – – – A/B – – 4.34 – – – B – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. c Class Mass Weathering %Fa %Fs Pair Ice . a b Name DOM 03182DOM 03183 CM2DOM 03184 CM2DOM 03260 LL5DOM 03261 19.79 LL5 124.52DOM 03262 LL5 BDOM 03270 B LL5 1.85DOM 03271 308.5 LL5DOM 03272 215.4 A/B LL5 CDOM 03273 273.5 LL5 BDOM 03274 LL5 0–30 30.78 A/B 0–38DOM 03275 LL5 36.59 A/BDOM 03276 LL5 81.14 1–2 CDOM 03277 LL5 – 39.53 A –DOM 03278 LL5 34.53 – ADOM 03279 LL5 24.36 – – ADOM 03280 – LL5 – 25.53 B drm DOM 03281 – – LL6 16.07 B –DOM 03282 drm LL6 48.81 C – –DOM 03283 – LL5 – 41.08 – BDOM 03284 – L6 57.74 – mwit B/C –DOM 03285 L5 11.34 – A/B – –DOM 03286 – – L6 24.29 B – –DOM 03287 – – H5 mwit B – –DOM 03288 14.89 L3 mwit – – –DOM 03289 B/C L6 6.82 – – –DOM 03310 25.46 – mwit H5 C – – 25.15DOM 03311 – mwit C LL5 – –DOM 03312 20.24 mwit C LL5 – – –DOM 03313 36.01 – mwit B H5 – – 85.79DOM 03314 – mwit B H5 13.75 – –DOM 03315 mwit C L5 27.09 B/C – –DOM 03317 – mwit LL5 – B/C – 16.52LAP 02200 – mwit – L5 mwit – 15–29LAP 02201 C – 8.21 – LL5 –LAP 02202 7.97 12.6 6–24 C LL5 – –LAP 02203 mwit – – – LL5 CLAP 02208 11.39 – 4013.1 mwit – B/C – LL5 mwit LAP 02209 – 4820.9 B/C – LL5 A/B –LAP 02210 7277.3 – – LL5 A/B 20 mwit LAP 02211 mwit – – – 958.1 mwit LL5 A/BLAP 02213 1474.7 – mwit – LL5LAP 02214 1563.1 A/B – – 17 LL5 – A/BLAP 02218 2237.6 – – – mwit LL5 A/B –LAP 02230 1651.9 – mwit – – L4 A –LAP 02232 mwit 592.6 – – LL6 – A/B – 745.1 – LL6 mwit – A/B – – – 473.7 – A/B 218.7 – – – mwit – 230.9 – A/B mwit – mwit A/B – – mwit – – – A/B – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. Meteoritical Bulletin No. 89 A255 c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name LAP 02341LAP 02342 H6LAP 02343 CR2LAP 02344 LL5LAP 02345 LL5 103.66LAP 02346 LL5 42.42LAP 02347 A L5 14.35LAP 02348 A/B LL5 27.53LAP 02349 A/B CM2LAP 02350 A 9.37 CM2LAP 02351 14.08 B LL5 41.01LAP 02352 0–5 A/B LL5 18LAP 02353 6.86 A/B 26.01 LL6LAP 02354 B – L6 1–3 B 32.34LAP 02355 16 LL5 25.16LAP 02356 – A/B LL4 56.34LAP 02357 A/B – – L3 – –LAP 02358 A/B – 35.37 – H5 20.87LAP 02359 – – 0–3 B H5 – 0–45LAP 02360 A/B 1.71 – – H5 –LAP 02361 – 11.28 – A/B H5 – LAP 02362 – 39.85 – – B H5 –LAP 02363 13.43 – – B/C – H5 –LAP 02364 31.97 2269 – – B/C 2336 LL5 – LAP 02365 – 14.57 – – B/C – – LL6 – – LAP 02366 – B/C LL5 6.04 –LAP 02367 10.49 9–31 – L6 31.08 B/CLAP 02368 – – B/C LL6 – – – 24.08LAP 02369 A/B 1–18 – LL5 – – – 10.29LAP 02370 A/B H6 – –LAP 02371 A/B 19.41 – H5 – – –LAP 02372 1.09 – B/C LL5 – – –LAP 02373 – – 0.65 A/B – LL5 – –LAP 02374 – – B LL5 1.17 – –LAP 02375 – 213.2 L5 1.19 – CELAP 02376 – – – 181.13 LL5 – – CLAP 02377 B/C – – 167.97 LL5 B – –LAP 02378 – – LL5 – B 135.96LAP 02379 – – – 109.91 LL6 –LAP 02380 B – 103.63 – – LL6 A/B –LAP 02381 – – – 130.5 H6 – B –LAP 02382 – – LL5 – 88.69 –LAP 02383 A/B – Ure – – 85.51LAP 02384 – B – LL5 – – 162.78LAP 02385 B – – H6 75.96 –LAP 02386 – – C – – LL5 – 74.32 A – L5 – – 51.08 – B – – – – – B 35.04 – – – 40.68 – – C – – – A – 51.39 – – – – – B/C 12–21 – – – – – 15–18 – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name LAP 02283LAP 02284 LL5LAP 02285 L5LAP 02286 LL5LAP 02287 L5 37.09LAP 02288 LL5LAP 02289 A/B LL5 6.99LAP 02290 4.95 H5LAP 02291 B C L5 6.65 10.23LAP 02292 H5LAP 02293 B B 6.33 L5LAP 02294 – A/B LL5 9.74LAP 02295 H5 7.49 CLAP 02296 H6 3.49LAP 02297 C – 16.62 – – L5 16.47 CLAP 02298 B H5LAP 02299 – A/B – 17.38 L5 –LAP 02300 – – B/C – L5 8.17LAP 02301 LL5 – 7 C –LAP 02302 – – 17.75 LL5 –LAP 02303 – – 17.02 C – CM2 –LAP 02304 C 24 – – 108.45 A/B H5 9.07 – LAP 02305 – – – LL5 B – –LAP 02306 A – 9.23 – – L5 20LAP 02307 – 7.86 – – C L5 –LAP 02308 – B/C H5 9.93 – 13.46LAP 02309 – – – CM2 – – CLAP 02320 – – B 45.2 – – LL5LAP 02321 – – – LL5 – – 7.4 –LAP 02322 – B 1–34 – 14.15 LL5 8.42 –LAP 02323 – – C – LL5 34.27 B/C CLAP 02324 – 2626.4 LL5 –LAP 02325 – 1046 A/B – – – LL5 A/B – –LAP 02326 – – 452.7 – LL5 – LAP 02327 – 2269 A – 507.1 LL5 –LAP 02328 – – A/B 0–7 332.4 – LL5LAP 02329 – – A/B – – – 425.3 – LL5 –LAP 02330 A/B – 369.3 LL5 – –LAP 02331 – B – 254.4 LL5LAP 02332 – A/B – 432.2 – L5LAP 02334 – B 2269 – – – – 403.9 – L5LAP 02335 – – B – 218.49 – LL6LAP 02336 B – – – LL5 A/B 190.88LAP 02338 – – – – CM2 – 168.8LAP 02339 – – A/B – – – 135.09 L4 – LAP 02340 – – 180.1 C LL5 A/B – – – 85.56 LL5 A/B – – – – – – B – 218.25 – – 169.39 – – B – – A/B 65.44 – – – – – B – – – – – – – 0–42 – – – – – – – – – – – – – – – – 4–21 – 2336 – – – – – – – – – – – – – – Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. A256 S. S. Russell et al. c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name LAP 031381LAP 03569 Dio/OlLAP 03572 DioLAP 03573 LL6LAP 03583 1.89 LL5LAP 03587 B 813.7 LL5LAP 03593 525.4 UreLAP 03605 A 670.4 Iron ungLAP 03624 B 226.7 Iron ungLAP 03630 657.5 B 130.24 LL5LAP 03631 582.8 A/B Dio B 30 BLAP 03632 Iron ung BLAP 03637 165.67 Lunar B 27LAP 03645 164.9 25 175.67 LL5 30 ALAP 03677 92.57 R B ALAP 03718 – 10–25 – 3979 22 H5 BLAP 03719 25 229 – CM2 –LAP 03780 Aub-an –LAP 03782 – 127.56 – – – Aub A/BLAP 03784 44.75 – B 95.21 Euc-ub – – cnm 62.02LAP 03785 32–99 B/C CK5 fc – – BE –LAP 03979 B – – – CM2 3593 27–52 21.81 22.27MAC 02450 pve Dio/Ol 3593 pp pve – tlr MAC 02451 B/C A/B H5 24 2205 50.92 – – tlr MAC 02452 H5 7–43 43.43 bpt MAC 02453 B 1–48 LL5 18 2.41 3593 – BMAC 02454 2493.7 CK5 – B tlr MAC 02455 – tlr 0 L4 – 792.9 C pb MAC 02456 16 653.5 – H5 – –MAC 02457 410.4 C 2238 H5 A/B 30–58MAC 02458 – 3718 0 1762 L5 pve 33 1–40 AMAC 02459 – pve LL6 wbg 0 730.9MAC 02461 30 H6 cnm B 624.8 –MAC 02462 – B/C 2233 L5 739.5 – – –MAC 02463 205.63 pp B L5 wbg pve 25MAC 02464 – – B/C H5 A/B 3718 99.25MAC 02465 32 L5 – 3979 wbg –MAC 02466 97.41 C H5 pve MAC 02467 49.84 pp – – B/C H6 – – 26 33.3MAC 02468 B/C L3 –MAC 02472 33.96 – H5 – C – 29.6MAC 02474 – bl B/C – L5 – – – 16.74MAC 02475 H6 tn tn CMAC 02476 18.87 bl C – – H5 – – –MAC 02477 C H5 8.66 – – –MAC 02478 H5 2.57 C qm lmac – – H5 3.12 – – – – C – 6.63 tn – C jschm bl 6.8 C – 4–24 – – 5.85 – – – C 8.78 jschm C – j C – – bl – – – – – – bl hm 2467 – – – qm – – qm – hm – – – – – – qm – – – ci – – qm qm – – j – qm bl Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name LAP 02387LAP 02388 LL5LAP 02389 LL5LAP 02390 L5LAP 02391 LL5 38.76LAP 02392 LL5 24.67LAP 02393 B/C LL5LAP 02394 B 33.81 LL5 26.48LAP 02395 B/C L5LAP 02396 B 5.56 LL5 22.51LAP 02397 A L5LAP 02398 B 9.99 – LL5LAP 02399 B L5 8.58 18.05LAP 02400 – L5 –LAP 02401 B B 28.24 – L5 46.21LAP 02402 – B L5LAP 02403 B – 35.42 – LL5 –LAP 02404 – – C LL5 5.81LAP 02405 – 29.6 – L5 – LAP 02406 C – 30.15 – H5 36.37 –LAP 02407 B/C – – – – B/C L5LAP 02408 A/B – – 5.94 – – LL5LAP 02409 – 10.1 – A/B – LL5LAP 02410 – – – – LL5 8.72 – LAP 02411 B/C – – L5 – 8.31 40.52 CLAP 02412 – – – LL5 – 21.77 – LAP 02413 B/C – A/B – – LL5 – 22.9LAP 02414 A/B – – LL5 – –LAP 02415 – – – 77.48 122.46 B LL5 –LAP 02416 – – – 172.38 – B LL5 – BLAP 02417 LL5 B – 41.76 –LAP 02418 – – – – – L5 41.96 –LAP 02419 B – – – – – LL5 34.71LAP 02420 B – LL5 – – 44.25LAP 02421 – B/C – – – LL5LAP 02422 – B – – – LL5 – 3.08 54.63LAP 02423 – CM1 – 17.54LAP 02424 C – B – – – LL5 15.1LAP 02425 – B – – – H5 – – – 18.9LAP 02426 – – A L5 – –LAP 02427 1.99 B/C – L5LAP 02428 – – 6.23 B L5 – – – LAP 02429 – – A LL5 3.62 –LAP 031269 – – – – H5 6.05 CLAP 031370 – – – – Aub 7.56LAP 031372 C – Iron ung – – – 2.56 – 13.42 A – – Aub – – C A – – – 12.93 8.67 6.45 – – – B B – C – – 17.61 – – – – – B – – – – – – – – – – – – – 24 – – – – – – – – – – 21 – – 0 – – – – – – 2233 0 – – – – – – 2233 – – Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. Meteoritical Bulletin No. 89 A257 c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name MAC 02541MAC 02542 H5MAC 02543 H5MAC 02544 LL5MAC 02545 LL6 75.6MAC 02546 LL6 158.07MAC 02547 137.95 LL5 B/C B/CEMAC 02548 189.09 H5 A/BMAC 02549 L6 A/B 47.49MAC 02556 178.13 LL5 A/BMAC 02560 E3 A/BE 377.7MAC 02561 H5 – –MAC 02563 34.3 B/C H5 87.24 –MAC 02564 H5 – B/C A/BMAC 02565 H5 1.41 – –MAC 02566 – – H5 3.95 – CMAC 02567 H5 5.76 C – 20.42MAC 02568 L4 – C – –MAC 02569 – – C L5 0.4 – tn –MAC 02570 – qm H5 0.69 – 11.18MAC 02571 tm/umac B L4 – BMAC 02572 bl – C – H5 8.04 –MAC 02573 – 14.4 – H5 bl mtl – A/B 92.13MAC 02574 L4 – – A/B 0–1MAC 02575 14.13 B – L5 lmac MAC 02576 – – B L5 9.99 –MAC 02577 – lmac L5 9.55 bl B/C – –MAC 02579 – – – H5 5.89 B/C –MAC 02580 10.5 qm H5 B – –MAC 02581 – H5 2.79 – A/B –MAC 02582 hm 12.92 – – – L5 B/C –MAC 02584 hm B/CE – H6 4.56 schm – 18.76 –MAC 02585 – L4 B/C – – 19.42MAC 02586 B/C – – L4 bl MAC 02587 hm – C H5 – 0.43 hm – – –MAC 02589 – hm H6 0.32 B – –MAC 02590 15.65 – hm – LL5 BMAC 02591 A/B LL6 – 8.53 bl – – – –MAC 02592 LL6 2.52 – ssi C –MAC 02593 – – qm L4 0.92 C 0.66MAC 02594 – qm L5 58.3 B – –MAC 02595 – B L4 – 35.23 –MAC 02596 – qm – B lmac L5 – – BMAC 02597 48.68 – qm H5 oh –MAC 02598 36.17 A/B L5 – – –MAC 02599 64.02 qm B/C H6 – – – bl 72.9 B – L5 – 34.98 – hm B/C – – 25–28 58.15 C – – – – – bl A/B 0.61 – 2–22 qm qm – 1.58 – B – – C – – hm – – – – tm – – hm j – – – bl – – hm – bl – – – – – bl – – – lmac – bl – – hm tmac – – tm tm Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name MAC 02479MAC 02480 H6MAC 02481 H5MAC 02482 H6MAC 02483 H5MAC 02485 H4 0.38MAC 02486 H5 1.76 B/CMAC 02487 L4 1.04 CEMAC 02488 H5 2.53 CMAC 02489 L6 0.59 CMAC 02490 H5 4.03 CMAC 02491 10.48 L5 C – 17.56MAC 02492 C H5MAC 02493 20.86 – C H5MAC 02494 C H5 6.02 – 289.5 –MAC 02495 L4 347.9 C –MAC 02496 – B/C L4 124.45 –MAC 02498 C H4 188.78 – – B/C –MAC 02499 – LL5 – B/CMAC 02500 45.73 – bl – L6 –MAC 02501 56.51 B/C – L6 bl – – 18.86MAC 02502 B L3 – – 19.84 – –MAC 02503 qm B/C – H4 – A/BMAC 02504 qm 26.05 – – L4 – –MAC 02505 qm – B/C H6 – 5.52 – –MAC 02506 qm 32.38 – L5 – qm BMAC 02507 – – B H5 0.5 – qm MAC 02508 – – H5 7.69 – – hm –MAC 02509 – B H5 0.84 – B qm MAC 02510 qm 32.22 – – L3 – B 20.99MAC 02511 – B L5 – lmac – qm 12.02MAC 02513 – 1–25 B/C L5 jschm 136.77 – –MAC 02514 B/C H5 – B/C qm MAC 02515 62.41 L5 – –MAC 02516 – – – B H5 4.6 qm – – qm MAC 02517 H5 lmac 1.88 – –MAC 02518 2467 B/C – L4 2.65 – B/C bl MAC 02519 – lmac H5 4.49 – C – – 11.01MAC 02520 – H4 – CMAC 02523 qm 0–25 C H6 2.67 – –MAC 02524 – LL5 3.61 – C – 17.68 1–20MAC 02525 – H6 – bl A/B – –MAC 02526 ci C H6 9.62 – – 2467MAC 02528 hm LL6 9.46 – – B j j 3.54MAC 02529 sns – CV3 – C – hm MAC 02540 – – B/C H6 2.38 jschm LL6 0.24 24 C – – 0.22 – B – 5.61 – – B – lmac A/B 21 lmac 3.02 97.97 – – – – – C – A/B hm – – 4–17 hm – hm – – ci 0–3 – – – qm – – – j – 0–3 qm – – – – – – lmac j – – – – – hm bl – bl tn – – bl bl Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. A258 S. S. Russell et al. c 22.85 B – 1–4 – bl . rich ch Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name MAC 02665MAC 02668 LL6MAC 02669 H5MAC 02670 LL5MAC 02671 H5 2.16MAC 02672 H5 11.26MAC 02673 A/B H5 1.42MAC 02674 C L5 71.55MAC 02675 A/B L5 101.39 B/C Metal- B/C 53.66 17.2 B/C – 20.72 A/B – B/C – – – – – – – – – – – – tm – – – – tm bl – – – bl bl – tm – – tm bl MAC 02676MAC 02677 LL6MAC 02678 LL5MAC 02679 H5MAC 02680 199.3 H5MAC 02681 299.7 LL5 A/BMAC 02682 H5 A/B 55.68MAC 02683 LL5 17.73MAC 02684 B/C LL5 10.49MAC 02685 B/C L5 A/BMAC 02686 H5 3.8 30 3.4MAC 02687 L5 30 9.92MAC 02688 B/C H5 A/BMAC 02689 A/B 25 H5 1.81 –MAC 02690 25 L5 2.36 – A/BMAC 02691 – L6 0.18 B 14.15MAC 02692 – H4 – BMAC 02693 B/C – – LL6 0.77 – bl –MAC 02694 – H5 – 0.11 fi BMAC 02695 H6 0.38 – B –MAC 02696 – H6 2.08 – C tm – 0.24MAC 02698 – H6 – C – bl MAC 02699 C LL5 0.16 bl – – –MAC 02700 H6 0.12 – C –MAC 02701 H6 0.77 – – C tm –MAC 02702 bl CM2 0.31 – C – – tm 0.15MAC 02704 – H5 C –MAC 02705 C bl H5 0.4 – – – 10.68MAC 02706 – 10.11 H5 – – –MAC 02707 tm C C LL5 BE – – tm MAC 02708 bl LL5 4.45 – – – 12.55MAC 02709 – H5 C – – 57.97MAC 02710 bl C LL6 17.01 – – –MAC 02711 bl C – H5 – – B/C 0–41 7.94MAC 02712 bl – L5 –MAC 02713 bl – B/C – L4 1.19 bl – – 0.28 1–3 – H6 B – bl B 0.43 – – bl – – – 2.19 B – qm – – – – 1.06 C tn 1.74 bl – bl – B – – – C – – bl bl – – – – – – tm – – tm – – – tn – bl – – – bl – – – – bl tm – – – bl – qm – bl qm Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name MAC 02600MAC 02601 H5MAC 02602 L4MAC 02610 H5MAC 02611 H5 281MAC 02612 H5 328.3MAC 02613 H5 691.7 CMAC 02614 A/B LL5MAC 02616 C H5 2.6MAC 02617 H5 7.79 19.03MAC 02618 C H6 C 1.37MAC 02619 C H5MAC 02620 B/C L4 5.88 – –MAC 02621 L5 7.25 CMAC 02622 – H5 5.31 CMAC 02623 H5 3.98 – C –MAC 02624 – L5 8.06 C –MAC 02625 – – L4 3.03 – CE 44.8MAC 02626 H5 – C – 42.95MAC 02627 – L4 C – – lmac MAC 02628 30.54 qm C – – L5 – –MAC 02629 C H5 3.86 qm – 10.02MAC 02641 – L4 – – C –MAC 02642 – C – H5 hm 9.35 – –MAC 02643 qm 10.31 L5 qm – C – tm MAC 02644 C H5 0.07 – – –MAC 02645 – – H5 4.65 B –MAC 02646 hm – H5 2.58 C – –MAC 02647 qm H6 1.78 C – – –MAC 02648 lmac – – – H6 9.59 C 23.27MAC 02649 qm H5 – ci C – –MAC 02650 C – H6 3.18 – –MAC 02651 qm – – H5 7.63 C –MAC 02652 qm H6 2.59 – lmac C – –MAC 02653 H6 5.15 – C – qm –MAC 02654 – H6 0.2 C – –MAC 02655 ci H6 0.36 qm – – –MAC 02656 C – H6 0.36 – B/C –MAC 02657 qm H5 0.55 – B/C qm – –MAC 02658 H4 0.21 B/C – – –MAC 02659 tn – CM2 0.24 B/C – –MAC 02660 tn LL5 0.6 B/C – – –MAC 02661 tm L5 0.48 – – –MAC 02662 B/C – bl – LL6 0.45 B/C – 1.27 –MAC 02663 qm L5 bl B/C – – – 1.02 BMAC 02664 L5 – – – qm – B/C L5 3.81 – – – 2.69 hm B/C – – tm A/B – 5.4 – – – qm – 4.3 0–52 – – – C tn bl 3.02 – B/C bl – – B/C – – bl – – – – bl – bl – – – bl – – – – bl – – – bl bl – bl – – – – – bl tm – – – bl qm tm Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. Meteoritical Bulletin No. 89 A259 c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name MAC 02773MAC 02774 L5MAC 02775 H5MAC 02776 L4MAC 02777 H6MAC 02778 H5 6.7MAC 02779 L6 0.34MAC 02780 B CM2 0.61 BMAC 02781 L6 0.28 BMAC 02782 H5 0.15 BMAC 02783 L4 0.14 B 0.3MAC 02784 L4 BMAC 02785 L4 B 0.73MAC 02786 – L4 0.17 – BMAC 02787 10 L4 B –MAC 02789 H5 0.29 –MAC 02790 – B/C H6 2.69 – – BMAC 02791 1–39 LL5 1.29 B/C – –MAC 02792 LL5 1.23 – B/CMAC 02793 – LL5 0.7 – B/C – –MAC 02794 – H5 0.55 tn – – – 1.83MAC 02795 bl B H5 – B – 6.84MAC 02796 2779 bl B H5 – – – 6.6 –MAC 02797 bl B/C bl H5 – – 12.42 –MAC 02798 bl H5 – B/C –MAC 02799 bl C H5 4.61 – –MAC 02801 – H5 3.58 C – 15.29MAC 02802 – – bl LL5 C – –MAC 02803 bl – C – H5 0.87 – – tn 43.54MAC 02804 – H5 B – 21.48MAC 02805 – – tn C tn H5 13.85 –MAC 02806 – C – – tn H5 – A/BMAC 02807 tn H5 4.99 – –MAC 02808 – L4 0.09 C – –MAC 02809 – – – L5 0.06 qm – BMAC 02810 tm LL5 0.27 bl – B – bl 17.37 –MAC 02811 – H5 B –MAC 02812 – C – tm – – L5 7.57MAC 02813 H4 5.28 qm – C – 0.57MAC 02815 – H5 – B/C – 23.79MAC 02816 bl – B – – L4 –MAC 02817 qm 25.45 B/C H4 hm – – 46.01MAC 02818 A/B – LL5 – – 13.36MAC 02819 tm – B – – L5 bl –MAC 02820 B/C H4 bl 4.9 schm – – –MAC 02821 CM1-2 3.62 23.02 – – B/C – – H5 – B/C – A/B hm 3.76 – – – qm – 0.21 2.39 B/C – bl – – B – – – B tm 4.54 – qm – – – C – – qm – – bl – – bl – hm – – bl – – 2 – – – qm tm – – – – – – – qm qm bl – – qm – – bl qm – jschm Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name MAC 02714MAC 02715 H5MAC 02716 L5MAC 02717 H6MAC 02718 L5MAC 02719 L6 0.25MAC 02720 H6 1.11 BMAC 02721 H6 4.53 CMAC 02722 H5 0.97 CMAC 02723 L5 1.23 BMAC 02724 H5 0.2 CMAC 02725 H6 0.09MAC 02727 B L5 0.25 – BMAC 02728 L5 1.44 B – 11.84MAC 02729 H6 – CMAC 02730 C LL6 5.55 – –MAC 02731 L4 2.39 C – –MAC 02732 LL5 1.3 – CMAC 02733 – L5 2.24 – – – 7.51MAC 02734 C H6 C – – –MAC 02735 bl 10.12 A/B H4 13.34 – –MAC 02736 – bl – B/C LL6 – – BMAC 02737 bl L4 6.92 – – –MAC 02738 tm H5 2.87 – C –MAC 02739 bl – – L4 3.25 10.81 C –MAC 02740 31 – H5 bl B/C – – – A/BMAC 02741 bl 25.86 L4 – – – 26.72MAC 02744 qm B – H5 26 –MAC 02745 41.44 tm – C H5 qm – – 49.21MAC 02746 B H6 – 281.4 – –MAC 02747 hm C LL5 167.09 – – – –MAC 02748 – j – B/C EL4 – B/CMAC 02749 hm LL5 6.11 qm – – 16.31MAC 02755 hm 189.4 – L4 B/C – – – qm MAC 02760 – 140.71 – B/C CM2 A/BMAC 02761 hm – H5 B/C 18.52 –MAC 02762 – H5 – – – A/B –MAC 02763 12.76 – lmac – – H6 3.52MAC 02764 qm qm B/C H6 – umac – BMAC 02765 – H5 0.18 – – –MAC 02767 – – – L5 0.3 B – ci MAC 02768 L4 0.05 – j –MAC 02769 – B – L5 0.71 – B – lmac 1–4MAC 02770 – – H6 1.03 – qm B 1–40 lmac MAC 02771 L4 jschm 0.69 B –MAC 02772 – L5 0.77 – B – – hm L5 0.97 – – B – lmac bl 0.11 tm B – – 8.46 B – bl 1.44 – – – C – 0.7 – C tm – bl – – B – – – – – bl – – – – bl – – – tm – – – bl – – tm – – – bl – – tn – tn – – bl – tn tn – bl Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. A260 S. S. Russell et al. c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name MAC 02883MAC 02884 H5MAC 02885 L5MAC 02887 H5MAC 02888 L4MAC 02889 L4 0.07MAC 02890 L4 1.52 BMAC 02891 H5 2.05 CMAC 02892 H5 3.34 CMAC 02893 H5 1.27 BMAC 02894 L5 3.53 C 18.91MAC 02896 H5 A 14.18MAC 02897 B/C H6 – 52.09MAC 02898 B/C H5 –MAC 02899 21.38 B/C LL5 – 18.22MAC 02900 B/C H6 – –MAC 02901 B/C H5 1.84 – –MAC 02902 H5 1.52 – B – – 5.22MAC 02903 L5 – B – – 74.73MAC 02904 B/C H5 – – – 33.72MAC 02905 qm B/C H5 – – – – 28.62MAC 02906 bl B/C L4 – – –MAC 02907 bl 23.57 B/C H5 – – 31.99MAC 02908 ci B/C L4 – – – – 33.87MAC 02909 bl C LL5 – – – – ci MAC 02910 bl B/C LL5 9.77 – – ci MAC 02911 LL5 5.14 – – – B/C j MAC 02912 18.71 L4 – – 16.6 – B/C – bl MAC 02913 B L5 – – hm 2.67MAC 02914 A/B H6 – – 2.24MAC 02915 A/B – H5 – – – –MAC 02916 bl A/B LL5 4.86 – – ci –MAC 02917 bl L5 2.7 – B/C tm –MAC 02918 – L3 0.81 – – qm MAC 02919 B/C 308.1 – L4 0.35 – B – hm MAC 02920 – L5 – B A/B – qm MAC 02921 96.38 – L4 – – 222.16MAC 02922 B/C L4 – – qm 156.95 tm B –MAC 02923 – LL5 – 265.1 B/C –MAC 02924 qm L5 – – 106.68MAC 02925 hm C H5 – – – 177.2 B/CMAC 02926 – – 149.16 H5 – – qm lmac MAC 02928 B/C H5 – A/B – – 188.37 9–27 lmac MAC 02929 H5 194.96 – lmac B/CMAC 02930 – – – L4 2–24 – B/C 65.5MAC 02931 qm L4 – – 72.35 – – H5 B/C – tn 53.78 – – B/C – – – – tn 65.11 B/C bl – bl tn – – B – 9.03 lmac 29.34 – – – – B/C B/C lmac – – – – – – – qm – tn – – lmac qm – – – – – – – qm qm – – – – lmac – – lmac hm – – – lmac qm ci Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name MAC 02823MAC 02824 H5MAC 02825 H5MAC 02826 H5MAC 02827 H5MAC 02828 H5 0.04MAC 02829 L5 1.61 BMAC 02840 H5 4.62 CMAC 02841 H5 7.51 CMAC 02842 H5 0.16 CMAC 02843 H5 1.93 B 55.07MAC 02844 H5 B/CMAC 02845 C H5 6.51 –MAC 02846 LL5 8.12 B/C – 28.06MAC 02847 H5 B/C –MAC 02850 B/C H5 7.45 – – 18.06MAC 02851 L5 B/C – – – 4.25MAC 02852 B/C LL5 – 10.14MAC 02853 – A/B LL5 – – –MAC 02854 B/C H6 4.12 – – –MAC 02855 bl – CM2 2.93 – B/C – 1.38MAC 02856 qm – H5 B – – – 0.23MAC 02857 qm A H5 – – –MAC 02858 qm – B L5 3.37 – – 0.14MAC 02859 bl bl – H6 – C – C –MAC 02860 L4 0.19 – bl – –MAC 02861 bl L5 0.17 – – BMAC 02862 qm H6 1.87 – B – bl –MAC 02863 – H5 2.62 – C –MAC 02865 – qm L4 1.05 – C tm MAC 02866 1–2 L4 0.22 – – B – bl MAC 02867 – H6 1.66 B tm –MAC 02869 – H6 4.7 B –MAC 02870 – qm CM1 0.81 – – –MAC 02871 B/C – H5 0.13 B –MAC 02872 2779 bl – L5 0.6 bl – – BMAC 02873 bl L4 2.79 bl – 0.36 – –MAC 02874 B H6 B – – 16.97 BMAC 02875 hm L5 – – –MAC 02876 13.46 B/C – H5 – –MAC 02877 bl 12.59 A/B H5 – – – 38.7MAC 02878 bl B L5 – – –MAC 02879 96.76 bl – H6 B/C – 80.85MAC 02880 bl – B H5 – – – 30.33 –MAC 02881 ci B/C H5 – – –MAC 02882 23.47 bl B H6 – – 19.52 hm – B L5 qm – – – B/C – 7.53 – – – tn 0.61 – B/C bl – – 0.45 – B – – – tm 1.72 – B – qm – bl – C hm – – – – tm – – – – qm bl – – – – – – bl bl – – – – – bl – – bl schm – – tm – – qm – bl bl Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. Meteoritical Bulletin No. 89 A261 c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name PCA 02026PCA 02027 LL6PCA 02028 LL5PCA 02029 H5PCA 02030 106.79 L6PCA 02031 H5 A/B 98.44PCA 02032 H6PCA 02033 A/B 24.46 H5PCA 02034 10.39 B L5PCA 02035 13.76 B/C H5PCA 02036 B/C L5 3.73 –PCA 02037 46.4 H5 CPCA 02038 – 34.59 LL5 CPCA 02039 A/B H5 2.17 –PCA 02040 29.09 – H5 – CPCA 02041 22.39 – B/C H5 –PCA 02042 8.84 B/C L5PCA 02043 – B – LL6 1.66 – –PCA 02044 N 40 – LL5 9.41 – – – B/CPCA 02045 15.92 L4 N 40 BPCA 02046 C – H5 4.03 14.44 – – – –PCA 02047 H5 – – – N 40 –PCA 02048 B/C B N 40 9.18 L5PCA 02049 N 40 B – L6 1.21 – –PCA 02050 – – 23.76 LL6 – –PCA 02051 A/B – 25.47 N 40 C 18 CM2PCA 02052 N 40 40 N C – – H5 4.71 –PCA 02053 – – – H5 4.04 15.21 –PCA 02054 C – 16 N 40 N 40 LL5 9.78PCA 02055 C B N 40 – – – H5 25PCA 02056 20.76 B – – LL5 N 40 PCA 02057 – – 43.37 C – N 40 LL6 33.85PCA 02058 21 N 40 A/B – – – H6PCA 02059 B – L6 2.16 27.14 N 40 PCA 02065 – – – N 40 L5 40.79 CPCA 02066 – 0–40 – B N 40 – – – HowPCA 02067 A/B How 2.28 N 40 N 40 PCA 02068 – 18 – – H5 6.64 CPCA 02069 – – – 19.41 – LL6 N 40 PCA 02070 C 3.63 – B/C LL6 57.07 N 40 2011 17PCA 02071 – B 4751.3 – H5 – B/CPCA 02072 – – N 40 – – N 40 640.1 L5PCA 02073 C – N 40 244.2 – LL6PCA 02074 – B – LL5 518 – –PCA 02075 A/B – N 40 – 1175 LL5 – N 40 PCA 02076 – 1021.9 – L5 A/B – – 259.6 N 40 L5 B B/C – – – – 147.03 24–58 23–57 – – – A/B N 40 sw1 N 40 A/B 224.76 – – 2009 2009 – B/C 96.65 N 40 N 40 18 – – – N 40 B – – N 40 – N 40 – – 16 – – – – – – 40 N – – 40 N – 40 N – – N 40 – – – – N 40 – 40 N – me N 40 – N 40 – N 40 Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name MAC 02932MAC 02933 LL5MAC 02934 LL5MAC 02935 LL5MAC 02936 L5 25.65MAC 02937 H5 24.94 A/BMAC 02938 H5 13.24 A/BMAC 02939 LL5 A/BMAC 02940 10.12 H5MAC 02942 B/C LL5 8.01MAC 02943 H5 7.18 B/C 9.83MAC 02944 – L4 B/CMAC 02945 – A/B H4 8.21 19.16MAC 02946 – H5 B/C A/B 13.55MAC 02947 – L5 –MAC 02948 – B/C L4 2.12 –MAC 02949 – L4 4.7 B –MAC 02950 – L4 7.36 – –MAC 02951 B/C 44.13 – L5 lmac B/C – –MAC 02953 – 16.03 – B/C L5 lmac –MAC 02954 15.82 B H6 lmac – – –MAC 02955 18.02 B/C L5 – lmac –MAC 02956 – B/C H5 2.4 – –MAC 02957 qm – H4 6.29 – – – 15.09MAC 02958 C qm L4 – C lmac –MAC 02959 13.16 – C H5 –MAC 02960 lmac C – – H5 0.69 lmac – – – 15.06MAC 02961 LL5 – – C qm MAC 02962 12.48 C LL6 –MAC 02964 B H5 1.41 – – – –MIL 03346 qm – H6 5.45 – B qm – – 3.74MIL 03356 – qm B Nak qm 0.29MIL 03368 B/C – – – IVA 13.18MIL 03369 – B – – lmac Dio – qm PCA 02001 C – – 2.32 715.2 IIIC hm PCA 02002 – – 443.5 L5 CPCA 02003 – B L5 – – –PCA 02004 80.93 A – – – qm 119.96 H5 –PCA 02005 qm – B/C – qm L5 A 354PCA 02006 – L5 – qm – 451.3PCA 02020 – – – H5 – 308.6PCA 02021 hm C – C qm LL5 – 401.9PCA 02022 – – C LL6 lmac – 220.46PCA 02023 – 29 – – B LL5 21–49 – 661.6PCA 02024 ci B LL6 – – 77.98 hm PCA 02025 hm – C LL5 74.57 27 A/B – – tm H5 – 34.66 A/B – – hm – 67.11 – – A/B – 44.82 – qm A/B – – A/B – – 78.99 – – – – – B – – mit – – – – – – – – – N 40 – N 40 – – – N 40 – – N 40 – – – N 40 – – – N 40 N 40 – N 40 – – N 40 – N 40 N 40 – N 40 Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. A262 S. S. Russell et al. c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name QUE 02142QUE 02143 H5QUE 02144 H5QUE 02145 H5QUE 02146 L4QUE 02147 L6 2.19QUE 02148 L5 7.86 CQUE 02149 H6 5.93 CQUE 02158 LL5 0.83 CQUE 02160 Dio 1.2 CQUE 02161 LL5 4.6QUE 02162 12.14 C L5QUE 02163 1.32 C C H5 –QUE 02164 8.59 286.6 C H6 –QUE 02165 H5 B –QUE 02166 A/B 91.44 H5 – –QUE 02167 26.78 A/B H5 122.62 –QUE 02168 – B L5 –QUE 02169 B/C 82.82 – – H5 – –QUE 02170 50.99 – B/C LL4 –QUE 02171 60.66 gni – – C LL6 – –QUE 02172 sm 73.34 – B/C – H5 –QUE 02173 – 50.63 sm – B/C L5 58.48QUE 02174 22 – – mm – – B/C H5 24.9QUE 02175 A/B – – H5 – sm 99050 –QUE 02177 15.35 B/C – H5 gni sm mm QUE 02178 11.5 – – C – – LL5 – gni QUE 02179 LL5 6.04 mm – – – B/CQUE 02180 L5 5.88 – CQUE 02181 gni – – – – LL4 9.94 – CQUE 02182 1.9 H5 gni – – sm – CQUE 02183 0.55 H5 – B/CQUE 02184 gni – B – – LL5 3.17 51.54 –QUE 02185 – LL5 – mm – BQUE 02186 A/B sm 25.46 LL5 – –QUE 02187 sm 29.1 – B – H5 26.66 –QUE 02188 mm – L5 mm 14.45 – – BQUE 02189 A/B – H5 15.23 –RBT 03522 A/B gni – – LL4 –RBT 03523 A/B 37.88 – – CK5 sm – –RBT 03530 – B gni CM2 9.66 –RBT 03531 29.23 – – H5 27.09 B –RBT 03532 sm – – 282.4 B H5 – – –RBT 03533 A/B – sm – LL5 6.7 BRBT 03534 sm – gni – – LL5RBT 03535 23.13 – – H5 B gni – – 72.4 – – C gni H6 7.8 – gni – 42.6 – C – – 27–30 – sm B – 19 – – B gni rbm – 1–57 mm 9.87 – – – – B mm C – – – rbm – – – – – – gni – – gni – gni – – – – – – – – – – – – – – – – – – – – – Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name PCA 02077PCA 02078 LL6PCA 02079 LL5PCA 02080 H5QUE 02100 113.92 L6 02110H5136.62B/C–––rbm QUE 02101 LL5 B 25.61QUE 02102 LL5QUE 02103 B/C LL5 2.99 1007.5QUE 02104 11.5 H5 CQUE 02105 H5 B 02115H69.04B/C–––rbm QUE 02106 C 0.96 LL6QUE 02107 7.39 B H6 –QUE 02108 – B H5 4.33QUE 02109 LL5 9.86 CQUE 0.77 H5 – C –QUE 02111 – B 4.38 –QUE 02112 – 18.01 H5 CQUE 02113 0.79 C – LL4 – –QUE 02114 B – – H5 5.28 –QUE – N 40 H5 N 40 C –QUE 02116 19.51 – 12.12 –QUE 02117 – B/C – – H5 –QUE 02118 A/B – N 40 L4 6.42 – –QUE 02119 gni 12.97 N 40 – – LL5 B/C –QUE 02120 B/C – – – LL5 gni QUE 02121 LL5 4.62 mm – – –QUE 02122 – LL4 4.71 – B/C –QUE 02123 4.61 gni – – – LL4 A/BQUE 02124 3.88 sm A/B LL4 15.47 gni – –QUE 02125 – A/B – H6 – – 18.1QUE 02126 A/B sm – – LL4 gni QUE 02127 5.06 A/B LL5 18 10.36 gni –QUE 02128 – A/B LL4 – –QUE 02129 A/B – 11.25 sm – LL4 – 17.18QUE 02130 sm 16 B/C H4 gni –QUE 02131 A/B 3.8 – – LL5 –QUE 02132 5.43 – wsm LL5 – – A/BQUE 02133 gni 4.76 – B L5 – –QUE 02134 15.36 – – A/B H6 sm QUE 02135 1.26 – B LL4 – – – 11.55QUE 02136 – A/B gni H6 – –QUE 02137 gni A/B – – H5 5.39QUE 02138 mm – 12.85 LL4 mm – – B/CQUE 02139 8.68 – B/C – H5 – – gni QUE 02140 – B LL5 9.59 mm QUE 02141 18 – H5 1.82 gni – – B/C 5.49 – – – LL5 – B/C sm 10.56 A/B gni 16 – 1.3 – B/C – – 14.79 – gni – – 19.69 A/B C – – mm gni B – – – – gni – – – gni – gni – – – – – – sm – sm – – – – – gni – – gni – gni – – gni – sm – gni – – sm gni Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. Meteoritical Bulletin No. 89 A263 c el Ice; gni: Goodwin m: Canyonero Mesa (West MacAlpine Hills; PCA: Pecora f; SAN: Sandford Cliffs. uthwest #1; tlr: Terrapin Landing uthwest #1; tlr: Terrapin for explanation of columns. Forbidden Cove; fi: Fu Cliffs; schm: Schuttaine Moraine; sm: Scoraine Cliffs; Jacobs, pve: Pinnacle Vista Estates; qm: Quiche Jacobs, pve: Pinnacle Vista Trail; ci: Camp Ice; cn Trail; s: LAP: La Paz Icefield; MAC: i: Supersonic Icefield; sw1: So andra Range; RBT: Roberts Massi andra Range; RBT: . teoritical Bulletin No. 79 (1996) Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name SAN 03503SAN 03504 LL5SAN 03505 L5SAN 03506 LL5SAN 03507 LL4 43.7SAN 03508 LL5 7.35SAN 03509 B LL5 42.21 LL5 46.82 C B 44.3 B 67.79 B 22.71 A/B B – – – – – – – – – – – – – – mw – – – – sc sc – sc – sc sc – sc Nunataks; hm: Harvaine Moraine; j: Jacobs; jschm: Moraine; rbm: Round Bottom sc: Sandford Moraine; sns: snowshow ice; ss Royale; tm: That Moraine. Paradise Palms); drm: Dominion Range Main; fc: Escarpment; QUE: Queen Alex Abbreviations for meteorite name See “Notes to Table 2” in Me See “Notes to Table Icefield names: bl: Bottom Lip; bpt: Bridle Path Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions. a b c c . Class Mass Weathering %Fa %Fs Pair Ice Continued.

a b Name RBT 03536RBT 03537 H6RBT 03538 L5SAN 03480 L6SAN 03481 H5SAN 03482 L5 7.25SAN 03483 LL5 6.77 BSAN 03484 11.77 LL5 121.5SAN 03485 B/C LL5 B/CSAN 03486 61.75 160.17 C LL5SAN 03487 137.94 C H5 B/CSAN 03488 183.66 LL4 BSAN 03489 L5 B 76.08 –SAN 03500 – Euc-br –SAN 03501 B 79.36 H5 57.06SAN 03502 C – LL4 – – 29.19 A/B 89.42 – – L5 – A/B C – 17.33 – – 35.76 – – – C – – B/C – – 27.48 – – – – – C – – – – – mw – mw – – 48–59 sc – – – sc – – mw – – – – mw – – sc – – sc sc – – sc – – sc sc – sc Appendix 1. Recently described meteorites from the U.S. ANSMET expeditions.