Pyromorphite Don Shurtz, Pleasant Oaks Gem and Mineral Club of Dallas
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Download PDF About Minerals Sorted by Mineral Name
MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky. -
Plumbogummite Pbal3(PO4)2(OH)5 • H2O C 2001-2005 Mineral Data Publishing, Version 1
Plumbogummite PbAl3(PO4)2(OH)5 • H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 32/m. Crystals hexagonal or bladed, prismatic, to 5 mm, in parallel to subparallel aggregates; microscopically radially fibrous or spherulitic; usually as crusts, botryoidal, reniform, stalactitic, globular, compact massive. Physical Properties: Fracture: Uneven to subconchoidal. Tenacity: Brittle. Hardness = 4.5–5 D(meas.) = 4.01 D(calc.) = [4.08] Optical Properties: Transparent to translucent. Color: Grayish white, grayish blue, yellowish gray, yellowish brown, green, pale blue. Streak: White. Luster: Vitreous, resinous to dull. Optical Class: Uniaxial (+); segments of crystals may be biaxial. ω = 1.653–1.688 = 1.675–1.704 Cell Data: Space Group: R3m. a = 7.017(1) c = 16.75(1) Z = 3 X-ray Powder Pattern: Ivanhoe mine, Australia. 2.969 (10), 5.71 (9), 2.220 (8), 3.51 (7), 1.905 (6), 3.44 (5), 4.93 (4) Chemistry: (1) (2) SO3 0.67 P2O5 22.47 24.42 As2O5 0.04 Al2O3 25.45 26.32 Fe2O3 0.01 CuO 0.92 PbO 38.90 38.41 H2O [11.54] 10.85 Total [100.00] 100.00 1− (1) Ivanhoe mine, Australia; by electron microprobe, H2O by difference, (OH) • confirmed by IR; leading to Pb1.02Cu0.07Al2.92[(PO4)1.85(SO4)0.05]Σ=1.90(OH)5.29 0.73H2O. • (2) PbAl3(PO4)2(OH)5 H2O. Mineral Group: Crandallite group. Occurrence: An uncommon secondary mineral in the oxidized zone of lead deposits. Association: Pyromorphite, mimetite, duftite, cerussite, anglesite, wulfenite. Distribution: In France, from Huelgoat, Finist`ere.In England, from Roughton Gill, Red Gill, Dry Gill, and other mines, Caldbeck Fells, Cumbria; in Cornwall, from Wheal Gorland, Gwennap; at the Penberthy Croft mine, St. -
Mineralogical Study of the Advanced Argillic Alteration Zone at the Konos Hill Mo–Cu–Re–Au Porphyry Prospect, NE Greece †
Article Mineralogical Study of the Advanced Argillic Alteration Zone at the Konos Hill Mo–Cu–Re–Au Porphyry Prospect, NE Greece † Constantinos Mavrogonatos 1,*, Panagiotis Voudouris 1, Paul G. Spry 2, Vasilios Melfos 3, Stephan Klemme 4, Jasper Berndt 4, Tim Baker 5, Robert Moritz 6, Thomas Bissig 7, Thomas Monecke 8 and Federica Zaccarini 9 1 Faculty of Geology & Geoenvironment, National and Kapodistrian University of Athens, 15784 Athens, Greece; [email protected] 2 Department of Geological and Atmospheric Sciences, Iowa State University, Ames, IA 50011, USA; [email protected] 3 Faculty of Geology, Aristotle University of Thessaloniki, 54124 Thessaloniki, Greece; [email protected] 4 Institut für Mineralogie, Westfälische Wilhelms-Universität Münster, 48149 Münster, Germany; [email protected] (S.K.); [email protected] (J.B.) 5 Eldorado Gold Corporation, 1188 Bentall 5 Burrard St., Vancouver, BC V6C 2B5, Canada; [email protected] 6 Department of Mineralogy, University of Geneva, CH-1205 Geneva, Switzerland; [email protected] 7 Goldcorp Inc., Park Place, Suite 3400-666, Burrard St., Vancouver, BC V6C 2X8, Canada; [email protected] 8 Center for Mineral Resources Science, Department of Geology and Geological Engineering, Colorado School of Mines, 1516 Illinois Street, Golden, CO 80401, USA; [email protected] 9 Department of Applied Geosciences and Geophysics, University of Leoben, Leoben 8700, Austria; [email protected] * Correspondence: [email protected]; Tel.: +30-698-860-8161 † The paper is an extended version of our paper published in 1st International Electronic Conference on Mineral Science, 16–21 July 2018. Received: 8 October 2018; Accepted: 22 October 2018; Published: 24 October 2018 Abstract: The Konos Hill prospect in NE Greece represents a telescoped Mo–Cu–Re–Au porphyry occurrence overprinted by deep-level high-sulfidation mineralization. -
Twinning in Pyromorphite: the First Documented Occurrence of Twinning by Merohedry in the Apatite Supergroup
American Mineralogist, Volume 97, pages 415–418, 2012 Twinning in pyromorphite: The first documented occurrence of twinning by merohedry in the apatite supergroup STUART J. MILLS,1,2,* GIOVANNI FERRARIS,3 ANTHONY R. KAMPF,2 AND GEORGES FAVREAU4 1Geosciences, Museum Victoria, GPO Box 666, Melbourne 3001, Australia 2Mineral Sciences Department, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007, U.S.A. 3Dipartimento di Scienze Mineralogiche e Petrologiche, Università degli Studi di Torino, Via Valperga Caluso 35, I-10125 Torino, Italy 4421 Avenue Jean Monnet, 13090 Aix-en-Provence, France ABSTRACT We describe the first documented case of {1010} twinning by reflection (or by twofold rotation about [100]) or merohedry (class II) in a member of the apatite supergroup. Twinning about [100] had previously been noted for the apatite supergroup but not confirmed. Pyromorphite crystals from Puech de Compolibat, Combret, Aveyron, France, were studied by single-crystal X-ray diffraction 3 [a = 10.0017(19), c = 7.3413(16) Å, and V = 636.0(2) Å , in P63/m], where twinning was confirmed with the approximate twin fraction 62:38. Subsequent inspection of the morphology confirmed the nature of the twinning. The pyromorphite crystals are typically elongate and show the faces: (21 10), (2110), (0001), (0001), (1010), (1010), (101 2), and (1012). Keywords: Twinning by merohedry class II, pyromorphite, Puech de Compolibat, apatite supergroup, crystal structure INTRODUCTION and the center of symmetry 1 may always be considered as twin Twinning is the oriented association of two or more law. In class II twins, instead, the superimposed lattice nodes individuals that are related by a twin operation belonging to (and the corresponding superimposed diffracted intensities) are the point group either of the lattice (twinning by merohedry) not equivalent in the Laue group [e.g., crystal point group 6/m, or of a sublattice (twinning by reticular merohedry), but not Laue group 6/m, twin operation (1010) plane]. -
2012 Bmc Auction Specimens
A SAMPLER OF SELECTED 2017 BMC AUCTION SPECIMENS (2017 Auction Date is Saturday, 21 January) Volume 3 3+ Hematite [Fe 2O3] & Quartz [SiO2] Locality Cleator Moor Iron Mines Cleator Moor West Cumberland Iron Field Cumbria, England, UK Size 13.5 x 9.5 x 7.0 cm 1498 g Donated by Stonetrust Hematite Crystal System: Trigonal Photograph by Mike Haritos Physical Properties Transparency: Subtranslucent to opaque Mohs hardness: 6.5 Density: approx 5.3 gm/cm3 Streak: Red Luster: Metalic Vanadinite [Pb5(VO4)3Cl] var. Endlichite Locality Erupción Mine (Ahumada Mine) Los Lamentos Mountains (Sierra de Los Lamentos) Mun. de Ahumada Chihuahua, Mexico Size 12.0 x 9.5 x 7.0 cm 1134 g Donated by Stonetrust Crystal System: Hexagonal Physical Properties Transparency: Subtranslucent to opaque Mohs hardness: 3.5-4 Photograph by Mike Haritos Density: 6.8 to 7.1 gm/cm3 Streak: Brownish yellow Endlichite, Pb5([V, As]O4)3Cl, is the arsenic rich Luster: Adamantine variety of vanadinite with arsenic atoms (As) substituting for some of the vanadium (V) 2+ Dolomite [CaMg(CO3)2] & Chalcopyrite [CuFe S2] Locality Picher Field Tri-State District Ottawa Co. Oklahoma, USA Size 19.0 x 14.5 x 6.0 cm 1892 g Consigned with Reserve by Stonetrust Dolomite Crystal System: Trigonal Physical Properties Photograph by Mike Haritos Transparency: Transparent, Translucent, Opaque Mohs hardness: 3.5 to 4 Density: 2.8 to 2.9 gm/cm3 Streak: White Luster: Vitreous Calcite [CaCO3] Locality Mexico Size 15.5 x 12.8 x 6.2 cm 1074 g Donated by Stonetrust Calcite Crystal System: Trigonal Physical Properties Transparency: Transparent, Translucent Mohs hardness: 3 Density: 2.71 gm/cm3 Streak: White Luster: Vitreous, Sub-Vitreous, Photograph by Mike Haritos Resinous, Waxy, Pearly Quartz [SiO2], var. -
Arsentsumebite Pb2cu(Aso4)(SO4)(OH) C 2001-2005 Mineral Data Publishing, Version 1
Arsentsumebite Pb2Cu(AsO4)(SO4)(OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. As distorted crystals, to 2 mm, in aggregates and crusts. Twinning: Complex, observed. Physical Properties: Fracture: [Uneven] (by analogy to tsumebite). Tenacity: [Brittle.] Hardness = [3.5] D(meas.) = 6.46 D(calc.) = 6.39 Optical Properties: Semitransparent. Color: Grass-green to apple-green. Luster: [Vitreous.] Optical Class: Biaxial (–). Pleochroism: X = pale pistachio-green; Y = Z = bottle-green. α = 1.970 β = 1.992 γ = 2.011 2V(meas.) = 88◦ ◦ Cell Data: Space Group: P 21/m. a = 8.85 b = 5.92 c = 7.84 β = 112.6 Z=2 X-ray Powder Pattern: Tsumeb, Namibia; close to tsumebite. (ICDD 25-456). 3.25 (100), 4.80 (65), 2.76 (60), 3.64 (46), 2.96 (40), 3.01 (32), 2.094 (30) Chemistry: (1) (2) SO3 9.36 10.97 P2O5 0.55 As2O5 13.45 15.74 CuO 10.61 10.90 PbO 61.91 61.16 H2O 1.58 1.23 Total 97.46 100.00 (1) Tsumeb, Namibia; by electron microprobe, As2O5 originally given as As2O3, H2ObyCHN analyzer. (2) Pb2Cu(AsO4)(SO4)(OH). Mineral Group: Brackebuschite group. Occurrence: A rare mineral in the oxidized zone of a dolostone-hosted hydrothermal polymetallic ore deposit (Tsumeb, Namibia); in a hydrothermal polymetallic barite–fluorite deposit (Clara mine, Germany). Association: Malachite, cerussite, azurite, smithsonite, mimetite, bayldonite, conichalcite, duftite, quartz, iron oxide (Tsumeb, Namibia). Distribution: From Tsumeb, Namibia. In the Clara mine, near Oberwolfach, Black Forest, Germany. At Moldava, 20 km northwest of Teplice, Czech Republic. -
New Minerals Approved Bythe Ima Commission on New
NEW MINERALS APPROVED BY THE IMA COMMISSION ON NEW MINERALS AND MINERAL NAMES ALLABOGDANITE, (Fe,Ni)l Allabogdanite, a mineral dimorphous with barringerite, was discovered in the Onello iron meteorite (Ni-rich ataxite) found in 1997 in the alluvium of the Bol'shoy Dolguchan River, a tributary of the Onello River, Aldan River basin, South Yakutia (Republic of Sakha- Yakutia), Russia. The mineral occurs as light straw-yellow, with strong metallic luster, lamellar crystals up to 0.0 I x 0.1 x 0.4 rnrn, typically twinned, in plessite. Associated minerals are nickel phosphide, schreibersite, awaruite and graphite (Britvin e.a., 2002b). Name: in honour of Alia Nikolaevna BOG DAN OVA (1947-2004), Russian crys- tallographer, for her contribution to the study of new minerals; Geological Institute of Kola Science Center of Russian Academy of Sciences, Apatity. fMA No.: 2000-038. TS: PU 1/18632. ALLOCHALCOSELITE, Cu+Cu~+PbOZ(Se03)P5 Allochalcoselite was found in the fumarole products of the Second cinder cone, Northern Breakthrought of the Tolbachik Main Fracture Eruption (1975-1976), Tolbachik Volcano, Kamchatka, Russia. It occurs as transparent dark brown pris- matic crystals up to 0.1 mm long. Associated minerals are cotunnite, sofiite, ilin- skite, georgbokiite and burn site (Vergasova e.a., 2005). Name: for the chemical composition: presence of selenium and different oxidation states of copper, from the Greek aA.Ao~(different) and xaAxo~ (copper). fMA No.: 2004-025. TS: no reliable information. ALSAKHAROVITE-Zn, NaSrKZn(Ti,Nb)JSi401ZJz(0,OH)4·7HzO photo 1 Labuntsovite group Alsakharovite-Zn was discovered in the Pegmatite #45, Lepkhe-Nel'm MI. -
PPM Bi-Annual Report 2017 & 2018
PPM Bi-Annual Report 2017 & 2018 The Bi-Annual Report for the PPM Research Centre DEPARTMENT OF GEOLOGY UNIVERSITY OF JOHANNESBURG The Bi-annual Report of the PPM Research Centre for the two years 2017 and 2018, compiled by Jan Kramers. Layout and design by UJ Graphic Studio Special thanks/Acknowledgements We wish to extend a special word of thanks to all our corporate and governmental financial and logistical supporters (in alphabetical order): African Rainbow Minerals Anglo American Anglo Coal Anglo Gold Ashanti Anglo Platinum Anglo Research Assmang Assore Coaltech Council of Geoscience Cradle of Humankind Trust of Gauteng De Beers Consolidated Mines Department of Science and Technology (DST) Deutsche Akademische Austauschdienst (DAAD) Golder Associates Impala Platinum Kumba Iron Ore Lonmin National Research Foundation (NRF) Nkomati Joint Venture Rand Uranium (Gold One) Sibanye Stillwater South 32 Two Rivers Platinum Mine Vale Vedanta Resources Please direct all enquiries and proposals for research to: Dr Bertus Smith, Prof. Jan Kramers or Prof. Fanus Viljoen or PPM, Department of Geology University of Johannesburg Auckland Park Kingsway Campus PO Box 524, Auckland Park 2006 Johannesburg, South Africa E-mail: [email protected], [email protected] or [email protected] Tel: +27(0)11 559 4701 Fax: +27(0)11 559 4702 Cover photo: Product being poured at the ferrochrome smelter near Machadodorp. Photo B. Cairncross Header photo: The landscape at Aggeneys, Northern Cape. Photo: Trishya Owen-Smith Footer photo: Stalagmite Phalanx at Cango Caves. Photo: Trishya Owen-Smith Both footer and header photos were taken on the Honours field trip, September 2018. -
An Overview of the Type Mineralogy of Africa Florias Mees Geology
An overview of the type mineralogy of Africa Florias Mees Geology Department, Royal Museum for Central Africa, Tervuren Summary Out of the ca. 5500 valid mineral species that are currently known, about 400 have been initially described for localities in Africa. The first new mineral descriptions for this continent date from the late 18th century, but significant numbers have only been reached from the early 20th century onward. Up to now, the largest numbers of new species have been described for Namibia, the DR Congo, and South Africa, with a considerable lead over all other countries. In this overview of the type mineralogy of Africa, regional variations and the history of new mineral descriptions are covered, combined with a discussion of some general aspects of mineral species validity and mineral nomenclature, based on examples from Africa. Samenvatting – Een overzicht van de type mineralogie van Afrika Van de ca. 5500 geldige mineraalsoorten die momenteel gekend zijn, werden er ongeveer 400 voor het eerst beschreven voor vindplaatsen in Afrika. De eerste beschrijvingen van nieuwe mineralen voor dit continent dateren van het einde van de 18e eeuw, maar significante aantallen werden pas bereikt vanaf het begin van de 20e eeuw. Tot op heden werden de grootste aantallen nieuwe soorten beschreven voor Namibië, de DR Congo, en Zuid-Afrika, met aanzienlijke voorsprong op alle andere landen. In dit overzicht van de type mineralogie van Afrika worden regionale verschillen en de geschiedenis van de beschrijving van nieuwe mineralen overlopen, samen met een bespreking van enkele algemene aspecten van de geldigheid van mineraalsoorten en van de naamgeving van mineralen, aan de hand van voorbeelden uit Afrika. -
Descloizite Pbzn(VO4)(OH) C 2001-2005 Mineral Data Publishing, Version 1
Descloizite PbZn(VO4)(OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 2/m 2/m 2/m. As crystals, equant or pyramidal {111}, prismatic [001] or [100], or tabular {100}, with {101}, {201}, many others, rarely skeletal, to 5 cm, commonly in drusy crusts, stalactitic or botryoidal, coarsely fibrous, granular to compact, massive. Physical Properties: Fracture: Small conchoidal to uneven. Tenacity: Brittle. Hardness = 3–3.5 D(meas.) = ∼6.2 D(calc.) = 6.202 Optical Properties: Transparent to nearly opaque. Color: Brownish red, red-orange, reddish brown to blackish brown, nearly black. Streak: Orange to brownish red. Luster: Greasy. Optical Class: Biaxial (–), rarely biaxial (+). Pleochroism: Weak to strong; X = Y = canary-yellow to greenish yellow; Z = brownish yellow. Orientation: X = c; Y = b; Z = a. Dispersion: r> v,strong; rarely r< v.α= 2.185(10) β = 2.265(10) γ = 2.35(10) 2V(meas.) = ∼90◦ Cell Data: Space Group: P nma. a = 7.593 b = 6.057 c = 9.416 Z = 4 X-ray Powder Pattern: Venus mine, [El Guaico district, C´ordobaProvince,] Argentina; close to mottramite. 3.23 (vvs), 5.12 (vs), 2.90 (vs), 2.69 (vsb), 2.62 (vsb), 1.652 (vs), 4.25 (s) Chemistry: (1) (2) (1) (2) SiO2 0.02 ZnO 19.21 10.08 As2O5 0.00 PbO 55.47 55.30 +350◦ V2O5 22.76 22.53 H2O 2.17 −350◦ FeO trace H2O 0.02 MnO trace H2O 2.23 CuO 0.56 9.86 Total 100.21 100.00 (1) Abenab, Namibia. -
Journal of the Russell Society, Vol 4 No 2
JOURNAL OF THE RUSSELL SOCIETY The journal of British Isles topographical mineralogy EDITOR: George Ryba.:k. 42 Bell Road. Sitlingbourn.:. Kent ME 10 4EB. L.K. JOURNAL MANAGER: Rex Cook. '13 Halifax Road . Nelson, Lancashire BB9 OEQ , U.K. EDITORrAL BOARD: F.B. Atkins. Oxford, U. K. R.J. King, Tewkesbury. U.K. R.E. Bevins. Cardiff, U. K. A. Livingstone, Edinburgh, U.K. R.S.W. Brai thwaite. Manchester. U.K. I.R. Plimer, Parkvill.:. Australia T.F. Bridges. Ovington. U.K. R.E. Starkey, Brom,grove, U.K S.c. Chamberlain. Syracuse. U. S.A. R.F. Symes. London, U.K. N.J. Forley. Keyworth. U.K. P.A. Williams. Kingswood. Australia R.A. Howie. Matlock. U.K. B. Young. Newcastle, U.K. Aims and Scope: The lournal publishes articles and reviews by both amateur and profe,sional mineralogists dealing with all a,pecI, of mineralogy. Contributions concerning the topographical mineralogy of the British Isles arc particularly welcome. Not~s for contributors can be found at the back of the Journal. Subscription rates: The Journal is free to members of the Russell Society. Subsc ription rates for two issues tiS. Enquiries should be made to the Journal Manager at the above address. Back copies of the Journal may also be ordered through the Journal Ma nager. Advertising: Details of advertising rates may be obtained from the Journal Manager. Published by The Russell Society. Registered charity No. 803308. Copyright The Russell Society 1993 . ISSN 0263 7839 FRONT COVER: Strontianite, Strontian mines, Highland Region, Scotland. 100 mm x 55 mm. -
Colorado Ferberite and the Wolframite Series A
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OT1S SMITH, DIRECTOR .jf BULLETIN 583 \ ' ' COLORADO FERBERITE AND THE r* i WOLFRAMITE SERIES A BY FRANK L. HESS AND WALDEMAR T. SCHALLER WASHINGTON GOVERNMENT FEINTING OFFICE 1914 CONTENTS. THE MINERAL RELATIONS OF FERBERiTE, by Frank L. Hess.................. 7 Geography and production............................................. 7 Characteristics of the ferberite.......................................... 8 " Geography and geology of the Boulder district........................... 8 Occurrence, vein systems, and relations................................. 9 Characteristics of the ore.............................................. 10 Minerals associated with the ferberite................................... 12 Adularia.......................................................... 12 Calcite........................................................... 12 Chalcedony....................................................... 12 Chalcopyrite...................................................... 12 Galena........................................................... 12 Gold and silver.................................................... 12 Hamlinite (?).................................................... 14 Hematite (specular)................................................ 15 Limonite........................................................ 16 Magnetite........................................................ 17 Molybdenite..................................................... 17 Opal............................................................