DOCSLIB.ORG

European Journal of Mineralogy N° 4/2017 Contents

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
European Journal of Mineralogy N° 4/2017 Contents European Journal of Mineralogy N° 4/2017 Contents Preface: Chromitites, platinum-group elements, and ore minerals. A special issue dedicated to Zdenek Johan (1935-2016) .......... 539 Z. Johan , R.F. Martin , V. E itler. - Fluids are bound to be involved in the formation of ophiolitic chromite deposits .................. 543 Q. X iong , W.L. Griffin , J.-X. Huang , S.E.M. Gain , V. T oledo , N.J. P earson , S.Y. O’R eilly. - Super-reduced mineral assemblages in “ophiolitic” chromitites and peridotites: the view from Mount Carmel .............................................................. 557 F. Zaccarini , K.A. S ingh , G. Garuti , M. Satyanarayanan . - Platinum-group minerals (PGM) in the chromitite from the Nuasahi massif, eastern India: further findings and implications for their origin ........................................................................ 571 T. Auge , G. Morin , L. Bailly, T. Serafimovsky . - Platinum-group minerals and their host chromitites in Macedonian ophiolites 585 A. V ymazalovä , F. Laufek , S.F. Sluzhenikin , C.J. Stanley , V.V. K ozlov , D.A. C hareev , M.L. Lukashova . - Kravtsovite, PdAg2S, a new mineral from the Noril’sk-Talnakh deposit, Krasnoyarskiy kray, Russia............................................................ 597 F. Laufek , A. V ymazalovä , T.L. Grokhovskaya , J. PläSil, M. D uSek , D.A. O rsoev , V.V. K ozlov . - The crystal structure of sopcheite, Ag4Pd3Te4, from the Lukkulaisvaara intrusion, Karelia, Russia.................................................................................. 603 A.Y. B arkov , A.A. N ikiforov , N.D. T olstykh , G.I. Shvedov , V.N. K orolyuk . - Compounds of Ru-Se-S, alloys of Os-Ir, framboidal Ru nanophases, and laurite-clinochlore intergrowths in the Pados-Tundra complex, Kola Peninsula, R ussia ........ 613 J. Pa Sava , L. Ackerman , P. Halodovä , 0. Pour , J. D urisov A, F. Zaccarini , T. Aiglsperger , A. V ymazalovä . - Concentrations of platinum-group elements (PGE), Re and Au in arsenian pyrite and millerite from Mo-Ni-PGE-Au black shales (Zunyi region, Guizhou Province, China): results from LA-ICPMS study.................................................................................. 623 L.J. Cabri , M. K elvin , Z. Y ang , S.E. Jackson , O. A ltun . - Application of LA-ICP-MS trace-element analysis for precious metal deportment: a case study of the Kevitsa mine, Finland................................................................................................................. 635 E. Makovicky , S. K arup -Moller . - Exploratory studies of the Cu-Pd-Se system at 650 °C, 550 °C, 400 °C, and 300.......... °C 645 P. SkAcha , J. Sejkora , J. PlAsil. - Pfibramite, CuSbSe2, the Se-analogue of chalcostibite, a new mineral from Pribram, Czech Republic......................................................................................................................................................................................... 653 J. Sejkora , P. SkAcha , F. Laufek , J. PlASil. - Brodtkorbite, Cu2HgSe2, from Pribram, Czech Republic: crystal structure and description..................................................................................................................................................................................... 663 L. Bindi , W.H. Paar . - Jaszczakite, [(Bi,Pb)3S3][AuS2], a new mineral species from Nagybörzsöny, Hungary.............................. 673 N. M eisser, P. Roth , F. N estola , C. Biagioni , L. Bindi , M. Robyr . - Richardsollyite, TlPbAsS3, a new sulfosalt from the Lengenbach quarry, Binn Valley, Switzerland............................................................................................................................... 679 D. Topa , U. K olitsch , E. Makovicky , C. Stanley . - Ecrinsite, AgTl3Pb4AsnSb9S36, a new thallium-rich homeotype of baumhauerite from the Jas Roux sulphosalt deposit, Parc national des Ecrins, Hautes-Alpes, France........................................ 689 D. T opa , E. Makovicky , B. Stoeger , C. Stanley . - Heptasartorite, Tl7Pb22As55S108, enneasartorite, Tl6Pb32As70S140and hendekasartorite, Tl2Pb48As82S172, three members of the anion-omission series o f‘sartorites’ from the Lengenbach quarry at Binntal, Wallis, Switzerland....................................................................................................................................................... 701 P. O rlandi , C. Biagioni , E. Bonaccorsi , Y. M oelo , W.H. Paar . - Lead-antimony sulfosalts from Tuscany (Italy). XXI. Bemarlottiite, Pb12(As10Sb6)zS16S36, a new N = 3.5 member of the sartorite homologous series from the Ceragiola marble quarry: occurrence and crystal structure............................................................................................................................. 713 K. B reiter, Z. K orbelov A, S. Chl Adek , P. U her , I. K nesl , P. Rambousek , S. Honig , V. S esulka . - Diversity of Ti-Sn-W- Nb-Ta oxide minerals in the classic granite-related magmatic-hydrothermal Cinovec/Zinnwald Sn-W-Li deposit (Czech Republic).................................................................................................................................. 727 C. Lerouge , E. Gloaguen , G. Wille, L. Bailly. - Distribution of In and other rare metals in cassiterite and associated minerals in Sn ±W ore deposits of the western Variscan Belt....................................................................................................................... 739 M. N ov Ak , J. Cicha , R. Copjakov A, R. Skoda , M.V. Galiov A. - Milarite-group minerals from the NYF pegmatite Velka skäla, Pisek district, Czech Republic: sole carriers of Be from the magmatic to hydrothermal stage .................................................... 755 S. Grangeon , F. Warmont , C. Tournassat , B. Lanson , M. Lanson , E. Elkaim , F. Claret . - Nucleation and growth of feitknechtite from nanocrystalline vemadite precursor................................................................................................................ 767 IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) - Newsletter 3 8 ................................................ Ill.
Load more

Recommended publications
  • Chromitites, Platinum-Group Elements, and Ore Minerals
    Eur. J. Mineral. 2017, 29, 539–541 Published online Chromitites, platinum-group elements, and ore minerals Special issue dedicated to Zdeněk Johan (1935–2016): Preface Fig. 1. Zdeněk Johan in the Mineralogical Collections at Charles University in Prague (Czech Republic). Zdeněk Johan, an outstanding Czech-French mineralogist and a great colleague, passed away in February 2016. He served as Scientific Director of the French Bureau de Recherches Géologiques et Minières (BRGM), became a fellow of professional and learned societies and received numerous honours and distinctions for his scientific achievements in mineralogy, crystal chemistry, petrology and ore geology (see Ettler, 2016). He also served in 1993 as president of the Société française de Minéralogie et de Cristallographie (SFMC), a founding society of the European Journal of Mineralogy (EJM). When asked by the Editorial Board, we thus immediately agreed to organize a special issue of EJM to celebrate Zdeněk Johan’s career. We were surprised by the feedback we received. We hope that the selection of papers, all following in the footsteps of Zdeněk Johan’s research activities, will resonate in the geoscience community. This special issue starts with Zdeněk’s late publication on the role of fluids in chromitite formation in ophiolite complexes (Johan et al., 2017), followed by an intriguing view on the origin of super-reduced mineral assemblages in ophiolite chromitites by Bill Griffin’s group (Xiong et al., 2017) and two articles on platinum-group minerals in ophiolites (Zaccarini et al., 2017; Augé et al., 2017). Platinum-group minerals occurring in different geological settings have always been a central theme in Zdeněk’s research and are represented here by several articles, which include the description of new minerals, new occurrences and analytical/experimental studies (Vymazalová et al., 2017; Laufek et al., 2017; Barkov et al., 2017; Pasava et al., 2017; Cabri et al., 2017; Makovicky & Karup-Møller, 2017).
    [Show full text]
  • 21Àxs34, a New Thallium Sulphosalt from Lengenbach Quarry, Binntal, Switzerland
    Mineralogical Magazine, December 2009, Vol.73(6), pp.1027–1032 Dalnegroite, Tl5ÀxPb2x(As,Sb)21ÀxS34, a new thallium sulphosalt from Lengenbach quarry, Binntal, Switzerland 1, 1 2 1 F. NESTOLA *, A. GUASTONI ,L.BINDI AND L. SECCO 1 Dipartimento di Geoscienze, Universita` degli Studi di Padova, Via Giotto 1, I-35137 Padova, Italy 2 Museo di Storia Naturale, sezione di Mineralogia, Universita` degli Studi di Firenze, Via La Pira, 4, I-50121 Firenze, Italy [Received 16 October 2009; Accepted 14 December 2009] ABSTRACT Dalnegroite, ideally Tl4Pb2(As12Sb8)S20S34, is a new mineral from Lengenbach, Binntal, Switzerland. It occurs as anhedral to subhedral grains up to 200 mm across, closely associated with realgar, pyrite, Sb- rich seligmanite in a gangue of dolomite. Dalnegroite is opaque with a submetallic lustre and shows a À2 brownish-red streak. It is brittle; the Vickers hardness (VHN25)is87kgmm (range: 69À101) (Mohs hardness ~3À3Ý). In reflected light, dalnegroite is highly bireflectant and weakly pleochroic, from white to a slightly greenish-grey. In cross-polarized light, it is highly anisotropic with bluish to green rotation tints and red internal reflections. According to chemical and X-ray diffraction data, dalnegroite appears to be isotypic with ˚ chabourne´ite, Tl5ÀxPb2x(Sb,As)21ÀxS34. It is triclinic, probable space group P1, with a = 16.217(7) A, b = 42.544(9) A˚ , c = 8.557(4) A˚ , a = 95.72(4)º, b = 90.25(4)º, g = 96.78(4)º, V = 5832(4) A˚ 3, Z =4. ˚ The nine strongest powder-diffraction lines [d (A)(I/I0)(hkl)] are: 3.927 (100) (2¯ 10 0); 3.775 (45) (22¯2); 3.685 (45) (4¯60); 3.620 (50) (440); 3.124 (50) (2¯8¯2); 2.929 (60) (42¯2); 2.850 (70) (4¯42); 2.579 (45) (0 14 2); 2.097 (60) (024).
    [Show full text]
  • Ralphcannonite, Agzn2tlas2s6, a New Mineral of the Routhierite
    1 1 Ralphcannonite, AgZn2TlAs2S6, a new mineral of the 2 routhierite isotypic series from Lengenbach, Binn 3 Valley, Switzerland 4 1* 2 3 5 LUCA BINDI , CRISTIAN BIAGIONI , THOMAS RABER , PHILIPPE 4 5 6 ROTH , FABRIZIO NESTOLA 7 8 9 10 1 Dipartimento di Scienze della Terra, Università degli Studi di Firenze, Via G. La Pira, 4, I- 11 50121 Firenze, Italy 12 2 Dipartimento di Scienze della Terra, Università di Pisa, Via Santa Maria, 53, I-56126 Pisa, 13 Italy 14 3 FGL (Forschungsgemeinschaft Lengenbach), Edith-Stein-Str. 9, D-79110 Freiburg, 15 Germany 16 4 FGL (Forschungsgemeinschaft Lengenbach), Ilanzhofweg 2, CH-8057 Zurich, Switzerland 17 5 Dipartimento di Geoscienze, Università di Padova, Via Gradenigo, 6, I-35131 Padova, Italy 18 19 20 21 22 *e-mail address: [email protected] 23 2 24 ABSTRACT 25 The new mineral species ralphcannonite, AgZn2TlAs2S6, was discovered in the Lengenbach 26 quarry, Binn Valley, Wallis, Switzerland. It occurs as metallic black equant, isometric to 27 prismatic crystals, up to 50 μm, associated with dufrénoysite, hatchite, realgar, and baryte. 28 Minimum and maximum reflectance data for COM wavelengths in air are [λ (nm): R (%)]: 29 471.1: 25.8/27.1; 548.3: 25.2/26.6; 586.6: 24.6/25.8; 652.3: 23.9/24.8. Electron microprobe 30 analyses give (wt%): Cu 2.01(6), Ag 8.50(16), Zn 10.94(20), Fe 3.25(8), Hg 7.92(12), Tl 31 24.58(26), As 18.36(19), Sb 0.17(4), S 24.03(21), total 99.76(71).
    [Show full text]
  • Crystallography of Sartorite from Binn. ( with Plate V.) by Cnaal~8 0
    212 Crystallography of Sartorite from Binn. ( With Plate V.) By CnAaL~8 0. T~CHX~AN~, Ph.D., F.G.8. [Read June 12, 1906.] LITERATURE J. ~. yore Rath, ' Mineraloglsche Mittheilungen (Fortsetzuug III): If. Skleroklas.' Ann. Chem. Phys. (Poggendorff), 1864, vol. cxxii, pp. 880-387. H. Baumhauer, ' Ueber den Skleroklas yon Binn.' Sitzungsber. k. preuss. Akad. Wiss. Berlin, 1895, pp. 243-252. R. H. Solly, ' Sulpharsenites of lead fl'om the Binnenthal.' Min. Mag., 1900, vol. xii, pp. 282-297 (Sartorite on pp. 286 and 297). Translation in Zeits. Kryst. Min., 1891, vol. xxxv, pp. 321-344~. W. J. Lewis, ' A large crystal of sulpharsenite of lead from the Binnenthal.' Min. Mag., 1908, vol. xiii, p. xxxiv. (Analysis by H. Jackson.) R. H. Solly, 'On sartorite . and other minerals from the Binnenthal." Min. Mag., 1904, vol. xiv, p. xx. (Title only; abstract, giving angular elements, in ' Nature,' 1903, vol. lxlx, p. 142.) lI. Baumhauer, ' Die Minerallen des Binnenthals.' Bull. Murlthienne, Soc. valais. sci. nat., 1905, p. 85-49. HE mineral sartorite (of Dana) or scleroclase (of v. Waltershausen) T appears to have been found much more frequently in latter years in the well-known dolomite at the Lengenbach, in the Binnenthal, Switzerland, than was formerly the case, and it may now be considered to be one of the commonest of the group of sulpharsenites of lead which have made this locality famous. I~rge, detached, longitudinally striated, prismatic crystals, mostly devoid of terminal faces, have been especially frequent, the majority of which are doubtless sartorites. Notwithstanding this abundance of material, there still exists some {Toubt respecting the system in which this mineral crystallizes.
    [Show full text]
  • A Specific Gravity Index for Minerats
    A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951).
    [Show full text]
  • Hendekasartorite Tl2pb48as82s172
    Hendekasartorite Tl2Pb48As82S172 Crystal Data: Monoclinic. Point Group: 2/m. As imperfectly formed crystals. Physical Properties: Cleavage: Good on {100}. Tenacity: Brittle. Fracture: Conchoidal. Hardness = 3-3.5 VHN = 208-221 214 average (25 g load). D(meas.) = n.d. D(calc.) = 5.18 Optical Properties: Opaque. Color: Lead-gray; gray-white in reflected light, deep red internal reflections rare. Streak: Dark brown. Luster: Metallic. Anisotropism: Moderate to weak in brown-violet and deep green tints. Bireflectance: Weak. Pleochroism: Weak. Optical Class: n.d. R1-R2: (400) 39.5-42.5, (420) 38.7-41.8, (440) 38.0-41.3, (460) 37.5-40.8, (470) 37.2-40.6, (480) 37.1-40.4, (500) 36.7-40.0, (520) 36.2-39.5, (540) 35.6-38.9, (546) 35.3-38.5, (560) 35.0-38.1, (580) 34.3-37.2, (589) 33.9-36.8, (600) 33.4-36.3, (620) 32.6-35.3, (640) 31.8-34.4, (650) 31.5-34.0, (660) 31.1-33.6, (680) 30.5-32.9, (700) 30.1-32.4 Cell Data: Space Group: P21/c. a = 31.806(5) b = 7.889(12) c = 28.556(4) β = 99.034(2)° Z = 1 X-ray Powder Pattern: Calculated pattern. 3.50 (100), 2.941 (76), 2.753 (73), 2.751 (73), 3.87 (69), 2.947 (66), 9.76 (56) Chemistry: (1) (2) Tl 2.80 1.86 Pb 44.63 45.18 Sb 0.90 As 27.10 27.91 S 24.83 25.05 Total 100.26 100.00 (1) Lengenbach quarry, Binntal, Wallis, Switzerland; average of 22 electron microprobe analyses; corresponds to Tl3.03Pb47.71(As80.10Sb1.65)Σ=81.74S171.52.
    [Show full text]
  • Guettardite Pb(Sb, As)2S4 C 2001-2005 Mineral Data Publishing, Version 1
    Guettardite Pb(Sb, As)2S4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. As acicular crystals, to 2 mm, the faces of which are irregularly streaked parallel to the axis of elongation; also as small anhedral grains. Twinning: Polysynthetic twinning on {100}, common in polished section. Physical Properties: Cleavage: Perfect on {001}. Fracture: Conchoidal. Tenacity: Very brittle. Hardness = n.d. VHN = 180–197 (50 g load). D(meas.) = 5.26 D(calc.) = 5.39 Optical Properties: Opaque. Color: Grayish black; in polished section, white with reddish internal reflections. Luster: Metallic. Pleochroism: Relatively strong. R1–R2: (470) 37.6–42.6, (546) 36.1–41.2, (589) 34.8–39.3, (650) 32.8–36.7 ◦ 0 Cell Data: Space Group: P 21/a. a = 20.05(5) b = 7.95(2) c = 8.44(2) β = 101 46(10) Z=8 X-ray Powder Pattern: Madoc, Canada. 3.52 (100), 2.795 (90), 4.19 (50), 3.90 (50), 2.670 (50), 2.653 (50), 2.335 (40) Chemistry: (1) (2) (3) Pb 38.8 38.50 38.94 Cu 0.49 Sb 24.1 23.57 22.88 As 12.2 13.61 14.08 S 24.1 23.46 24.10 Total 99.2 99.63 100.00 (1) Madoc, Canada; by electron microprobe, corresponding to Pb1.01(Sb1.07As0.88)Σ=1.95S4.05. (2) Pitone quarry, Italy; by electron microprobe; corresponding to Pb1.04Cu0.04 (Sb1.00As0.94)Σ=1.94S3.78. (3) Pb(Sb, As)2S4 with Sb:As = 1:1.
    [Show full text]
  • Rathite Ag2pb12-Xtlx/2As18+X/2S40
    Rathite Ag2Pb12-xTlx/2As18+x/2S40 Crystal Data: Monoclinic. Point Group: 2/m. Crystals prismatic to short prismatic and striated parallel to [100]. Twinning: Polysynthetic on {001}in some material. Physical Properties: Cleavage: Perfect on {001}; parting on {010}. Fracture: Subconchoidal. Hardness = 3 VHN = 161 D(meas.) = 4.986-5.446 (varies with Tl content) D(calc.) = 5.31 Optical Properties: Not fully opaque. Color: Lead-gray, may tarnish to iridescence; grayish white in reflected light with deep red internal reflections. Streak: Chocolate-brown. Luster: Metallic to dull. Pleochroism: Strong. Anisotropism: Intense; olive-green or yellow and bluish violet. R1-R2: (400) 40.0-45.2, (420) 39.2-44.8, (440) 38.4-44.3, (460) 37.8-43.7, (480) 37.2-43.7, (500) 36.6-42.8, (520) 36.0-42.3, (540) 35.4-41.8, (560) 34.7-41.0, (580) 34.0-40.2, (600) 33.3-39.3, (620) 32.6-38.4, (640) 31.9-37.6, (660) 31.3-36.7, (680) 30.7-35.9, (700) 30.2-35.2 Cell Data: Space Group: P21/c. (Tl-poor) a = 8.471(2) b = 7.926(2) c = 25.186(5) β = 100.58(3)° Z = 1; (Tl-rich) a = 8.521(2) b = 8.005(2) c = 25.031(5) β = 100.56(3)° Z = 1 X-ray Powder Pattern: Binntal, Switzerland. 2.75 (100), 3.60 (80), 3.39 (70), 2.87 (70), 4.19 (60), 2.97 (60), 2.22 (50) Chemistry: (1) (2) (3) Pb 36.61 47.24 27.33 Tl 5.36 0.16 11.78 Ag 4.13 3.35 3.75 As 27.31 21.76 29.28 Sb 1.94 3.89 2.16 S 24.48 23.55 25.35 Total 99.82 99.95 99.65 (1) Binntal, Switzerland; by electron microprobe, average of 11 analyses; corresponds to Ag2.00Tl1.36Pb9.24(As19.08Sb0.84)Σ=19.92S40.00.
    [Show full text]
  • Baumhauerite, a New Mineral; and Dufrenoysite
    151 Sult)harsenites of Lead from the JBinnenthal x Part III.--Baumhauerite, a new mineral; and Dufrenoysite. By tL tL Soz~Y, M~.. With an analysis by H. JAcxso~, M.A. [Read November 12, 1901.] Be~,-h~uerite', 4PbS.Shs,Ss. OR this new mineral I propose the name baumhauerite in honour ]~ of Dr. H. Baumhauer, Professor of 311neralogy in the University of Frelburg, Switzerland, who has done so much to elucidate this com- plicated group of sniphareenltes of lead. CRYSTALLOGRAPHY. System: Oblique. a : b : c ---- 1.186817 : 1 : 0.947168; ~ = 82~ '. These elements are calculated from the angles 100:101--50~ ', 101:001 -- 82 ~ 15~' and 010 :llI -----50~ ' measured on crystal No. I. The crystals closely resemble dufrenoyslte and jordanite in appearance. They may be distinguished from dufrenoysite by the marked oblique development of the zone [100,001], and from jordanite by the absence of twin striations and by the colour of the streak. The edges in the pyramid zone and between planes in the zone [100,010] are more or less rounded. The orthopinacoid (100), which is the direction of cleavage, is always largely developed and has a brilliant lustre ; it is sometimes finely striated parallel to the axis of symmetry, and some- times shows unsymmetrical markings. The best developed zone on the crystals is [100,001]. The prism zone [100,010] is sometimes deeply furrowed as in rathlto and dufrenoysite. Sometimes similar ldanes on opposite sides of (010) give different angles ; thiA may pos- sibly be due to twinning about a plane making a small angle with (100), i Part L--General Dese~.'l~ien and Chemlcal z,~lyae~, with a CryStallographic account of Jordan;ha.
    [Show full text]
  • 29 2003 Auth Indexword.Indd
    American Mineralogist, Volume 88, pages i–x, 2003 2003 Author Index Akaogi, M., see Sugawara and Akaogi, 1020 Baron, D., see Drouet et al., 1949 crystal-chemical characterization, 464 Alberti, A., Fois, E., and Gamba, A.: A mo- Barrès, O., see Pelletier et al., 1801 Bindi, L., see Bonazzi et al., 223 lecular dynamics study of the behavior of Barrett, S., see Bickmore et al., 709 Bindi, L., see Bonazzi et al., 1796 sodium in low albite, 1 Barron, L.M.: A simple model for the pres- Binu-Lal, S.S., see Santosh et al., 1689 Alcock, J., Myer, K., and Muller, P.D.: Three- sure preservation index of inclusions in Bird, D.K., see Fridriksson et al., 277 dimensional model of heat flow in the diamond, 1615 Bird, D.K., see Fridriksson et al., 1060 aureole of the Marcy anorthosite, Adiron- Barrón, V., Torrent, J., and Grave, E.: Hydroma- Bird, D.K., see Neuhoff et al., 410 dack Highlands, New York: Implications ghemite, an intermediate in the hydrother- Bish, D.L., see Dera et al., 1428 for depth of emplacement, 474 mal transformation of 2-line ferrihydrite Bish, D.L., see Fridriksson et al., 277 Allan, N.L., see Lavrentiev et al., 1522 into hematite, 1679 Bish, D.L., see Fridriksson et al., 1060 Allwardt, J.R., Lee, S.K., and Stebbins, J.F.: Bass, J.D., see Wang et al., 1608 Bish, D.L., see Hou et al., 167 Bonding preferences of non-bridging O at- Baxter, G., see Lesher et al., 1181 Bish, D.L., Vaniman, D.T., Chipera, S.J., and oms: Evidence from 17O MAS and 3QMAS Beane, R.J., see Bostick et al., 1709 Carey, J.W.: The distribution of zeolites and
    [Show full text]
  • Sulfosalt Systematics: a Review
    Eur. J. Mineral. 2008, 20, 7–46 Published online February 2008 Sulfosalt systematics: a review. Report of the sulfosalt sub-committee of the IMA Commission on Ore Mineralogy Yves MOËLO1,*, Secretary, Emil MAKOVICKY2,**, Associate Secretary, Nadejda N. MOZGOVA3, past President of the Sulfosalt Sub-Committee, John L. JAMBOR4,Nigel COOK5,Allan PRING6,Werner PAAR7, Ernest H. NICKEL8,Stephan GRAESER9,Sven KARUP-MØLLER10,Tonciˇ BALIC-ŽUNIC2, William G. MUMME8,Filippo VURRO11,Dan TOPA7,Luca BINDI12, Klaus BENTE13 and Masaaki SHIMIZU14 1 Institut des Matériaux Jean Rouxel, UMR 6502 CNRS-Université de Nantes, 2, rue de la Houssinière, 44 322 Nantes Cedex 3, France *Corresponding author, e-mail: [email protected] 2 Department of Geography and Geology, University of Copenhagen, Østervoldgade 10, 1350 Copenhagen, Denmark **Corresponding author, e-mail: [email protected] 3 IGEM, Russian Academy of Sciences, Staromonetny per. 35, Moscow 109017, Russia 4 Leslie Research and Consulting, 316 Rosehill Wynd, Tsawwassen, B.C. V4M 3L9, Canada 5 Natural History Museum (Geology), University of Oslo, Postboks 1172 Blindern, 0318 Oslo, Norway 6 South Australian Museum, Department of Mineralogy, North Terrace, Adelaide, South Australia 5000, Australia 7 Department of Materials Engineering and Physics, University of Salzburg, Hellbrunnerstraße 34, 5020 Salzburg, Austria 8 CSIRO-Exploration & Mining, PO Box 5, Wembley, Western Australia 6913, Australia 9 Naturhistorisches Museum, Augustinerstraße 2, 4001 Basel, Switzerland 10 Institute of Mineral Industry, Danish
    [Show full text]
  • The Lengenbach Quarry in Switzerland: Classic Locality for Rare Thallium Sulfosalts
    Research Collection Review Article The Lengenbach Quarry in Switzerland: Classic Locality for Rare Thallium Sulfosalts Author(s): Raber, Thomas; Roth, Philippe Publication Date: 2018-09 Permanent Link: https://doi.org/10.3929/ethz-b-000302136 Originally published in: Minerals 8(9), http://doi.org/10.3390/min8090409 Rights / License: Creative Commons Attribution 4.0 International This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library minerals Review The Lengenbach Quarry in Switzerland: Classic Locality for Rare Thallium Sulfosalts † Thomas Raber 1,* and Philippe Roth 1,2 1 Lengenbach Research Association (Forschungsgemeinschaft Lengenbach, FGL), Gemeinde Binn, Dorfstr. 11, 3996 Binn, Switzerland 2 Swiss Seismological Service, ETH Zurich, Sonneggstr. 5, 8092 Zurich, Switzerland; [email protected] * Correspondence: [email protected] † Anniversary publication—60 years of continuous mineral search at Lengenbach and 15 years of FGL. Received: 11 July 2018; Accepted: 6 September 2018; Published: 14 September 2018 Abstract: The Lengenbach quarry is a world-famous mineral locality, especially known for its rare and well-crystallized Tl, Pb, Ag, and Cu bearing sulfosalts. As of June 2018, it is the type locality for 44 different mineral species, making it one of the most prolific localities worldwide. A total of 33 thallium mineral species have been identified, 23 of which are type minerals. A brief description of several thallium species of special interest follows a concise and general overview of the thallium mineralization. Keywords: Lengenbach; Binn valley; thallium; sulfosalts; hutchinsonite; fangite; richardsollyite; sartorite; routhierite-stalderite; chabournéite-dalnegroite 1. Introduction The Lengenbach quarry in the Binn valley, Valais, Switzerland (Figures1 and2) is located in Triassic meta-dolomites of the Penninic zone in the Swiss Alps.
    [Show full text]