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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. -
Barite (Barium)
Barite (Barium) Chapter D of Critical Mineral Resources of the United States—Economic and Environmental Geology and Prospects for Future Supply Professional Paper 1802–D U.S. Department of the Interior U.S. Geological Survey Periodic Table of Elements 1A 8A 1 2 hydrogen helium 1.008 2A 3A 4A 5A 6A 7A 4.003 3 4 5 6 7 8 9 10 lithium beryllium boron carbon nitrogen oxygen fluorine neon 6.94 9.012 10.81 12.01 14.01 16.00 19.00 20.18 11 12 13 14 15 16 17 18 sodium magnesium aluminum silicon phosphorus sulfur chlorine argon 22.99 24.31 3B 4B 5B 6B 7B 8B 11B 12B 26.98 28.09 30.97 32.06 35.45 39.95 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 potassium calcium scandium titanium vanadium chromium manganese iron cobalt nickel copper zinc gallium germanium arsenic selenium bromine krypton 39.10 40.08 44.96 47.88 50.94 52.00 54.94 55.85 58.93 58.69 63.55 65.39 69.72 72.64 74.92 78.96 79.90 83.79 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 rubidium strontium yttrium zirconium niobium molybdenum technetium ruthenium rhodium palladium silver cadmium indium tin antimony tellurium iodine xenon 85.47 87.62 88.91 91.22 92.91 95.96 (98) 101.1 102.9 106.4 107.9 112.4 114.8 118.7 121.8 127.6 126.9 131.3 55 56 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 cesium barium hafnium tantalum tungsten rhenium osmium iridium platinum gold mercury thallium lead bismuth polonium astatine radon 132.9 137.3 178.5 180.9 183.9 186.2 190.2 192.2 195.1 197.0 200.5 204.4 207.2 209.0 (209) (210)(222) 87 88 104 105 106 107 108 109 110 111 112 113 114 115 116 -
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. -
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. -
Tungsten Minerals and Deposits
DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Bulletin 652 4"^ TUNGSTEN MINERALS AND DEPOSITS BY FRANK L. HESS WASHINGTON GOVERNMENT PRINTING OFFICE 1917 ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 25 CENTS PER COPY CONTENTS. Page. Introduction.............................................................. , 7 Inquiries concerning tungsten......................................... 7 Survey publications on tungsten........................................ 7 Scope of this report.................................................... 9 Technical terms...................................................... 9 Tungsten................................................................. H Characteristics and properties........................................... n Uses................................................................. 15 Forms in which tungsten is found...................................... 18 Tungsten minerals........................................................ 19 Chemical and physical features......................................... 19 The wolframites...................................................... 21 Composition...................................................... 21 Ferberite......................................................... 22 Physical features.............................................. 22 Minerals of similar appearance................................. -
Mottramite, Descloizite, and Vanadinite) in the Caldbeck Area of Cumberland
289 New occurrences of vanadium minerals (mottramite, descloizite, and vanadinite) in the Caldbeck area of Cumberland. By ART~VR W. G. KINGSBURu F.G.S., Dept. of Geology and Mineralogy, University Museum, Oxford, and J. HARTLnY, B.Sc., F.G.S., Dept. of Geology, University of Leeds. [Taken as read 10 June 1954.] Summary.--Four new occurrences of vanadium minerals are described. New X-ray powder data are given for descloizite and mottramite, and show appreciable differences. Evidence is brought that the original occurrence of mottramite was not at Mottram St. Andrew, Cheshire, but Pim Hill, Shropshire, and that most if not all specimens labelled Mottram St. Andrew or Cheshire really came from Pim Hill. ANADIUM minerals are rare in the British Isles, and only two V species, mottramite (Cu, Zn)PbV0tOH and vanadinite Pbs(VO4)aC1, have so far been recorded from a limited number of localities. We do not include the vanadiferous nodules from Budleigh Salterton in Devon, as the vanadiferous mineral has not been identified. Mottramite, supposedly from Mottram St. Andrew in Cheshire, was first described in 1876,1 but we have evidence (below, p. 293) that the locality was in fact Pim Hill in Shropshire. ~ Vanadinite has so far only been found at Leadhills and Wanlockhead in Scotland. Vauquelinite has been de- scribed from Leadhills and Wanlockhead,a but the specimens have since been shown to be mottramite. 4 As a result of our investigations in the Lake District, we have found several new localities in the Caldbeck area for raottramite, deseloizite, and vanadinite. Higher part of Brandy Gill, Carroek Fell. -
Barite–Celestine Geochemistry and Environments of Formation Jeffrey S
Barite–Celestine Geochemistry and Environments of Formation Jeffrey S. Hanor Department of Geology and Geophysics Louisiana State University Baton Rouge, Louisiana 70803 INTRODUCTION Minerals in the barite (BaSO4)–celestine (SrSO4) solid solution series, (Ba,Sr)SO4, occur in a remarkably diverse range of sedimentary, metamorphic, and igneous geological environments which span geological time from the Early Archean (~3.5 Ga) to the present. The purpose of this chapter is to review: (1) the controls on the chemical and isotopic composition of barite and celestine and (2) the geological environments in which these minerals form. Some health risks are associated with barite, and these are discussed near the end of this chapter. Although complete solid solution exists between BaSO4 and SrSO4 most representa- tives of the series are either distinctly Ba-rich or Sr-rich. Hence, it is convenient to use the term barite to refer to not only the stochiometric BaSO4 endmember but also to those (Ba,Sr)SO4 solid solutions dominated by Ba. Similarly, the term celestine will refer here not only to the stoichiometric SrSO4 endmember but to solid solutions dominated by Sr. Such usage is in accord with standard mineral nomenclature. The Committee on Mineral Names and Nomenclature of the International Mineralogical Association recognizes “celestine” as the official name for SrSO4. However, the name “celestite” is still commonly used in the literature. Geological significance of barite and celestine Most of the barite which exists in the Earth’s crust has formed through the mixing of fluids, one containing Ba leached from silicate minerals, and the other an oxidized shallow fluid, such as seawater, which contains sulfate. -
Mimetite Pb5(Aso4)3Cl C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Hexagonal
Mimetite Pb5(AsO4)3Cl c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 6/m. Crystals are usually prismatic to acicular k [0001], to 12 cm, may be tabular, showing {1010}, {0001}, {1011}, rarely {1121}, {2131}, others; rounded, barrel-shaped, mammillary, stalactitic, granular. Twinning: On {1122}, very rare. Physical Properties: Cleavage: On {1011}, interrupted. Fracture: Uneven to subconchoidal. Tenacity: Brittle. Hardness = 3.5–4 D(meas.) = 7.24 D(calc.) = 7.26 Piezoelectric; may fluoresce reddish yellow under LW or SW UV. Optical Properties: Transparent to translucent. Color: Pale to bright yellow, yellowish brown, yellow-orange, white, may be colorless; colorless or pale yellow in transmitted light. Streak: White. Luster: Resinous to subadamantine. Optical Class: Uniaxial (–), commonly anomalously biaxial (–), sectored. Pleochroism: Weak. Absorption: O < E. ω = 2.147 = 2.128 Cell Data: Space Group: P 63/m (synthetic). a = 10.250(2) c = 7.454(1) Z = 2 X-ray Powder Pattern: Synthetic. 3.06 (100), 3.01 (90), 2.962 (66), 3.36 (38), 2.110 (30), 1.994 (22), 1.905 (20) Chemistry: (1) (2) P2O5 0.14 As2O5 23.17 23.17 PbO 74.58 74.99 Cl 2.39 2.38 −O=Cl2 0.54 0.54 Total 99.74 100.00 (1) Phoenixville, Pennsylvania, USA. (2) Pb5(AsO4)3Cl. Polymorphism & Series: Dimorphous with clinomimetite. Mineral Group: Apatite group. Occurrence: A common secondary mineral in the oxidized zone of arsenic-bearing lead deposits. Association: Cerussite, anglesite, smithsonite, willemite, pyromorphite, wulfenite. Distribution: Many localities. A few for well-crystallized material include: Johanngeorgenstadt, Saxony, Germany. -
Minerals Found in Michigan Listed by County
Michigan Minerals Listed by Mineral Name Based on MI DEQ GSD Bulletin 6 “Mineralogy of Michigan” Actinolite, Dickinson, Gogebic, Gratiot, and Anthonyite, Houghton County Marquette counties Anthophyllite, Dickinson, and Marquette counties Aegirinaugite, Marquette County Antigorite, Dickinson, and Marquette counties Aegirine, Marquette County Apatite, Baraga, Dickinson, Houghton, Iron, Albite, Dickinson, Gratiot, Houghton, Keweenaw, Kalkaska, Keweenaw, Marquette, and Monroe and Marquette counties counties Algodonite, Baraga, Houghton, Keweenaw, and Aphrosiderite, Gogebic, Iron, and Marquette Ontonagon counties counties Allanite, Gogebic, Iron, and Marquette counties Apophyllite, Houghton, and Keweenaw counties Almandite, Dickinson, Keweenaw, and Marquette Aragonite, Gogebic, Iron, Jackson, Marquette, and counties Monroe counties Alunite, Iron County Arsenopyrite, Marquette, and Menominee counties Analcite, Houghton, Keweenaw, and Ontonagon counties Atacamite, Houghton, Keweenaw, and Ontonagon counties Anatase, Gratiot, Houghton, Keweenaw, Marquette, and Ontonagon counties Augite, Dickinson, Genesee, Gratiot, Houghton, Iron, Keweenaw, Marquette, and Ontonagon counties Andalusite, Iron, and Marquette counties Awarurite, Marquette County Andesine, Keweenaw County Axinite, Gogebic, and Marquette counties Andradite, Dickinson County Azurite, Dickinson, Keweenaw, Marquette, and Anglesite, Marquette County Ontonagon counties Anhydrite, Bay, Berrien, Gratiot, Houghton, Babingtonite, Keweenaw County Isabella, Kalamazoo, Kent, Keweenaw, Macomb, Manistee, -
Quaternary Celestine and Gypsum Extensional Veins in a Folded Hypersaline Lake Infill: the Qaidam Basin, Wes- Tern China
© Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at Austrian Journal of Earth Sciences Volume 103/2 Vienna 2010 Quaternary celestine and gypsum extensional veins in a folded hypersaline lake infill: the Qaidam basin, wes- tern China Franz NEUBAUER1)*), Yongjiang LIU2), Johann GENSER1), Andrea Brigitte RIESER1)3), Gertrude FRIEDL1), Xiaohong GE2) & Martin THÖNI4) 1) Dept. Geography and Geology, University of Salzburg, Hellbrunnerstr. 34, A-5020 Salzburg, Austria; KEYWORDS 2) Faculty of Earth Sciences, Jilin University, 130061 Changchun, China; Sr isotopic stratigraphy 3) present address: Nagra, Hardstrasse 73, 5430 Wettingen, Switzerland; extensional vein 4) Dept. of Lithospheric Research, Vienna University, Althanstr. 14, A-1090 Vienna, Austria; Qaidam basin celestine *) Corresponding author, [email protected] brine Abstract The nonmarine, at present hypersaline Qaidam basin of Western China comprises a ca. 8–17 km thick sedimentary fill, which is dominated by Eocene to Recent clastic rocks. These successions were folded due to ongoing India-Eurasia convergence from late Miocene onwards until today. Shortening also resulted in enhanced fluid flow and precipitation of sulphate minerals in subvertical tension gashes, which are mainly filled by celestine and fibrous gypsum. The orientation of subvertical veins is similar over most parts of the western Qaidam basin and indicates NNE-SSW to N-S shortening (present-day coordinates) dissimilar to the NE-motion direction deduced from recent geodetic (GPS) data. In deeper stratigraphic levels of anticlinal cores, tension gashes composed of fibrous gypsum subparallel to bedding demonstrate fluid overpressure during their formation at a shallow structural level, below the conversion temperature of gypsum to anhydrite. -
A SAMPLER of SELECTED 2018 BMC AUCTION SPECIMENS Auction Date: Saturday, January 20, 2018 Snow Date: June 9, 2018 Volume 004 Bismuth(Bi) Xls
A SAMPLER OF SELECTED 2018 BMC AUCTION SPECIMENS Auction Date: Saturday, January 20, 2018 Snow date: June 9, 2018 Volume 004 Bismuth(Bi) xls. (Lab. Grown) Unusually large size l 9.0 x 8.6 x 8.2 cm l 360 g l Germany l Donated by l Mike Haritos Photograph by Mike Haritos Albite NaAlSi3 O8, Sodium aluminum silicate l 22 x 15.5 x 8.0 cm l 2,243 g l Hohe Tauern, Carinthia, Austria l BMC purchase Photograph by Mike Haritos Gypsum var. Selenite CaSO4 · 2H2O Hydrated Calcium Sulfate, Calcite CaCO3, Calcium Carbonate & Quartz SiO2 Silicon dioxide l 19.3 x 16.0 x 11.1 cm l 2,146 g l Cavnic Mine (Kapnikbánya), Cavnic (Kapnic; Kapnik), Maramures Co., Romania. l BMC Purchase Photograph by Mike Haritos Rhodochrosite (slab) MnO3 Manganese Carbonate l 19.0 x 11.1 x.3.0 cm l 1,130 g l Capillitas Mine, Andalgalá Department, Catamarca, Argentina l BMC Purchase Photograph by Mike Haritos Celestine (Celestite) SrSO4, Strontium Sulfate l 12.4 x 10.5 x 6.7 cm l 879 g l Madagascar l BMC Purchase Photograph by Mike Haritos Quartz var. Chalcedony SiO2 Silicon Dioxide l 12.4 x 10.5 x 6.7 cm l 879 g l Idar Oberstein, Hunsrück, Rhineland-Palatinate, Germany l BMC Purchase Photograph by Mike Haritos Rhodochrosite MnCO3 Manganese Carbonate with minor Pyrite FeS2 Iron Sulfide l 12.5 x 8.0 x 6.8 cm l 818 g l Huanzala Mine, Huallanca, Huallanca District, Bolognesi Province, Ancash Department, Peru l BMC Purchase Photograph by Mike Haritos Wulfenite PbMoO4, Lead Molybdate l 8.0 x 6.0 x 3.5 cm l 177 g l Bleiberg District, Gailtaler Alpen & Karnische Alpen, Carinthia, Austria (Type Locality) l BMC Purchase Photograph by Mike Haritos Uvarovite Ca3Cr2(SiO4)3, Calcium Chromium Silicate l 10.0 x 8.5 x 5.4 cm l 809 g l Outokumpu Cu-Co- Zn-Ni-Ag-Au ore field, Eastern Finland Region, Finland l BMC Purchase Photograph by Mike Haritos Copper Cu, Elemental Copper & CaCO3, Calcium Carbonate l 7.1 x 5.0 x 2.5 cm l 106 g l Tsumeb Mine (Tsumcorp Mine), Tsumeb, Otjikoto Region (Oshikoto), Namibia l BMC Purchase Photograph by Mike Haritos Quartz var.