Ore Petrography, Geochemistry, and Genesis of Epithermal Silver-Gold Veins
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Washington State Minerals Checklist
Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite -
Gomposition and Occurrence of Electrum Atthe
L37 The Canadian M inerala g i st Vol.33,pp. 137-151(1995) GOMPOSITIONAND OCCURRENCEOF ELECTRUM ATTHE MORNINGSTAR DEPOSIT, SAN BERNARDINOCOUNTY, GALIFORNIA: EVIDENCEFOR REMOBILIZATION OF GOLD AND SILVER RONALD WYNN SIIEETS*, JAMES R. CRAIG em ROBERT J. BODNAR Depanmen of Geolngical Sciences, Virginin Polytechnic h stitate and Stale (Jniversity, 4A44 Dening Hall, Blacl<sburg, Virginin 24060, U.S-A,. Arsrnacr Elecfum, acanthiteand uytenbogaardtite have been examined from six depthswithin the tabular quartzt calcite sockwork and breccia-filled veins in the fault-zone-hostedMorning Star depositof the northeasternMojave Desert, Califomia. Six distinct types of electrum have been identified on the basis of minerat association,grain moryhology and composition. Two types, (1) p1'rite-hostedand (2) quartz-hostedelectrum, occur with acanthite after argentite and base-metalsulfide minerals in unoxidized portions of the orebody; the remaining forr types, (3) goethite-hostedelectrum, (4) electnrm cores, (5) electrumrims and (6) wire electrum,are associatedwith assemblagesof supergeneminerals in its oxidizedportions. Pyrite- hosted quartz-hostedand goethite-hostedelectrum range in compositionfrom 6l ta 75 utt.7oAu and have uniform textures and no zoning. In lower portions ofthe oxidized ore zone, electrum seemsto replacegoethite and occursas small grains on surfacesof the goethite.Textural evidencefavors supergeneremobilization of Au and Ag, which were depositedas electrum on or replacinggoethite. This type of electrumis identical in appearanceand compositionto prinary electrum,In the upper portions of the oxidized zone,secondary electum occursas a gold-rich rim on a core of elechum and as wire-like grains,both with acanthiteand uytenbogaardtite.Such secondaryelectrum contains from 78 to 93 wt./o Au. Textural relations and asso- ciated minerals suggestthat the primary electrum was hydrothermally depositedand partially remobilized by supergene processes. -
Preliminary Results of Hydrothermal Alteration Assemblage
Preliminary Results of Hydrothermal Alteration Assemblage Classification in Aurora and Bodie Mining Districts, Nevada and California, with Airborne Hyperspectral Data Amer Smailbegovic, James V. Taranik and Wendy M. Calvin Arthur Brant Laboratory for Exploration Geophysics University of Nevada, Reno ABSTRACT The Aurora and Bodie mining districts are located in Bodie Hills, north of Mono Lake, on opposite sides of the Nevada-California state line. From the standpoint of economic geology, both deposits are structurally controlled, low-sulfidation, adularia-sericite precious metal vein deposits with an extensive alteration halo. The area was exploited from the late 1870’s until 1988 by both underground and minor open pit operations (Aurora), exposing portions of ore-hosting altered andesites, devitrified rhyolites as well as quartz-adularia-sericite veins. Much of the geologic mapping and explanation was ad- hoc and primarily in support of the mining operations, without particular interest paid to the system as a whole. The University of Nevada, Reno has acquired both high- and low- altitude AVIRIS data of the region. Low-altitude data was acquired in July 2000, followed by high-altitude collection in October 2000. The AVIRIS coverage was targeted on the main vein system in Aurora (Prospectus and Humboldt Vein), East Brawley Peak prospect (midpoint between Aurora and Bodie) and “Bonanza Zone” (Bodie Bluff and Standard Hill) in Bodie, where the hydrothermal alteration zones appear to be the most pervasive. The ground-observations and mining/prospecting reports suggest propylitic alteration throughout the Bodie Hills, argillic and potassic alteration in Aurora and Bodie, (low-sulfidation system) and alunitic alteration (high-sulfidation system) on East Brawley Peak. -
Acanthite Ag2s C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Monoclinic, Pseudo-Orthorhombic
Acanthite Ag2S c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic, pseudo-orthorhombic. Point Group: 2/m. Primary crystals are rare, prismatic to long prismatic, elongated along [001], to 2.5 cm, may be tubular; massive. Commonly paramorphic after the cubic high-temperature phase (“argentite”), of original cubic or octahedral habit, to 8 cm. Twinning: Polysynthetic on {111}, may be very complex due to inversion; contact on {101}. Physical Properties: Cleavage: Indistinct. Fracture: Uneven. Tenacity: Sectile. Hardness = 2.0–2.5 VHN = 21–25 (50 g load). D(meas.) = 7.20–7.22 D(calc.) = 7.24 Photosensitive. Optical Properties: Opaque. Color: Iron-black. Streak: Black. Luster: Metallic. Anisotropism: Weak. R: (400) 32.8, (420) 32.9, (440) 33.0, (460) 33.1, (480) 33.0, (500) 32.7, (520) 32.0, (540) 31.2, (560) 30.5, (580) 29.9, (600) 29.2, (620) 28.7, (640) 28.2, (660) 27.6, (680) 27.0, (700) 26.4 ◦ Cell Data: Space Group: P 21/n. a = 4.229 b = 6.931 c = 7.862 β =99.61 Z=4 X-ray Powder Pattern: Synthetic. 2.606 (100), 2.440 (80), 2.383 (75), 2.836 (70), 2.583 (70), 2.456 (70), 3.080 (60) Chemistry: (1) (2) (3) Ag 86.4 87.2 87.06 Cu 0.1 Se 1.6 S 12.0 12.6 12.94 Total 100.0 99.9 100.00 (1) Guanajuato, Mexico; by electron microprobe. (2) Santa Lucia mine, La Luz, Guanajuato, Mexico; by electron microprobe. (3) Ag2S. Polymorphism & Series: The high-temperature cubic form (“argentite”) inverts to acanthite at about 173 ◦C; below this temperature acanthite is the stable phase and forms directly. -
Porphyry Deposits
PORPHYRY DEPOSITS W.D. SINCLAIR Geological Survey of Canada, 601 Booth St., Ottawa, Ontario, K1A 0E8 E-mail: [email protected] Definition Au (±Ag, Cu, Mo) Mo (±W, Sn) Porphyry deposits are large, low- to medium-grade W-Mo (±Bi, Sn) deposits in which primary (hypogene) ore minerals are dom- Sn (±W, Mo, Ag, Bi, Cu, Zn, In) inantly structurally controlled and which are spatially and Sn-Ag (±W, Cu, Zn, Mo, Bi) genetically related to felsic to intermediate porphyritic intru- Ag (±Au, Zn, Pb) sions (Kirkham, 1972). The large size and structural control (e.g., veins, vein sets, stockworks, fractures, 'crackled zones' For deposits with currently subeconomic grades and and breccia pipes) serve to distinguish porphyry deposits tonnages, subtypes are based on probable coproduct and from a variety of deposits that may be peripherally associat- byproduct metals, assuming that the deposits were econom- ed, including skarns, high-temperature mantos, breccia ic. pipes, peripheral mesothermal veins, and epithermal pre- Geographical Distribution cious-metal deposits. Secondary minerals may be developed in supergene-enriched zones in porphyry Cu deposits by weathering of primary sulphides. Such zones typically have Porphyry deposits occur throughout the world in a series significantly higher Cu grades, thereby enhancing the poten- of extensive, relatively narrow, linear metallogenic tial for economic exploitation. provinces (Fig. 1). They are predominantly associated with The following subtypes of porphyry deposits are Mesozoic to Cenozoic orogenic belts in western North and defined according to the metals that are essential to the eco- South America and around the western margin of the Pacific nomics of the deposit (metals that are byproducts or poten- Basin, particularly within the South East Asian Archipelago. -
Silver-Rich Central Idaho
Silver-rich Disseminated Sulfides From a Tungsten-bearing Quartz Lode Big Creek District Central Idaho GEOLOGICAL SURVEY PROFESSIONAL PAPER 594-C Silver-rich Disseminated Sulfides From a Tungsten-bearing Quartz Lode Big Creek District Central Idaho By B. F. LEONARD, CYNTHIA W. MEAD, and NANCY CONKLIN SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 594-C Study of a low-grade tungsten deposit whose associated suljide minerals, extracted as waste, are rich in silver and contain some gold UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1968 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 35 cents (paper cover) CONTENTS Page Page Abstract __________________________________________ _ C1 Mineralogy and paragenetic sequence-Continued Introduction ______________________________________ _ 1 Alteration products ____________________________ _ C15 Location and operation _____________________________ _ 4 Paragenetic sequence ___________________________ _ 16 Geology __________________________________________ _ 4 Geologic thermometry __________________________ _ 18 Ore deposit _______________________________________ _ 5 Classification and origin of hypogene mineralization ____ _ 19 Mineralogy and paragenetic sequence ________________ _ 6 Oxidation and enrichment ___ ------------------------ 20 Typical ore ___________________________________ _ 6 Economic considerations ____________________________ _ 21 Gangue indicated by mill products _______________ _ 7 Acknowledgments ___________________ .:. ______________ _ 23 Tungsten minerals _______ ,______________________ _ 8 References ________________________________________ _ 23 Sulfides and related minerals ____________________ _ 8 ILLUSTRATIONS [Plates follow page C24f - PLATE 1. Drawing and X-ray micrographs of acanthite and copper sulfides on galena. 2. Drawing and X-ray micrographs of electrum in pyrite. 3. -
Revised Version the Crystal Structure of Uytenbogaardtite, Ag3aus2, And
Title The crystal structure of uytenbogaardtite, Ag3AuS2, and its relationships with gold and silver sulfides-selenides Authors Bindi, L; Stanley, Christopher; Seryotkin, YV; Bakakin, VR; Pal'yanova, GA; Kokh, KA Date Submitted 2017-03-30 1 1 1237R – revised version 2 The crystal structure of uytenbogaardtite, Ag3AuS2, and its relationships 3 with gold and silver sulfides-selenides 4 1, 2 3,4 5 5 LUCA BINDI *, CHRISTOPHER J. STANLEY , YURII V. SERYOTKIN , VLADIMIR V. BAKAKIN , 3,4 3,4 6 GALINA A. PAL’YANOVA , KONSTANTIN A. KOKH 7 8 1Dipartimento di Scienze della Terra, Università di Firenze, Via G. La Pira 4, I-50121Firenze, Italy 9 2Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom 3 10 Sobolev Institute of Geology and Mineralogy of the Siberian Branch of the Russian Academy of Sciences, pr. 11 Akademika Koptyuga, 3, Novosibirsk 630090, Russia 4 12 Novosibirsk State University, Pirogova str., 2, Novosibirsk 630090, Russia 5 13 Institute of Inorganic Chemistry, Siberian Branch of the RAS, prosp. Lavrentieva 3, 630090 Novosibirsk, Russia 14 15 * e-mail address: [email protected] 16 17 Abstract 18 The crystal structure of the mineral uytenbogaardtite, a rare silver-gold sulfide, was solved 19 using intensity data collected on a crystal from the type locality, the Comstock lode, Storey 20 County, Nevada (U.S.A.). The study revealed that the structure is trigonal, space group R 3 c, 3 21 with cell parameters: a = 13.6952(5), c = 17.0912(8) Å, and V = 2776.1(2) Å . The refinement 22 of an anisotropic model led to an R index of 0.0140 for 1099 independent reflections. -
Studies of Minerat Sutpho-Salts
STUDIESOF MINERATSUTPHO-SALTS: XIX_SEIENIANPOTYBASITE D. C. HARRIS.I E. W. NUFFIELD'2 eno M. H. FROHBERGB Ansrnecr A study of a rich Au-Ag ore from the La Guadalupe Arcos mine, Zacualpan, Mexico has led to the discovety of, selenian polybasite associated with a number of silver- bearing minerals. A cleavable variety of pyrite is a feature of the ore. The mineral occurs ur *i"""t" grains but about L milligram was concentrated from a more favourable material from the Sln Carlos mine, Guanajuato, Mexico. This gave the cell dimensions: o 13.00' b 7.5D, c 11.99A, p 90" and, by ,-ray spectroscopy, the approximate cell contents: (Agzs.eCus.z)'--flti" (Sb:.oAsr.e) (Srr.oSeo.o). 6*La-i. aiectasri'ncation of the polybasite-pearceite_minerals.Frondel's -7.5, classification"i"dv into two series, according to whether the cell is small (a*13, b c - L2), or double this, is unienable. The basic structural unit and external crystal fo-rm is the Lme for all polybasites and pearceites. Doubled dimensions, which manifest themselves as weak lntermediate layer lines on rotation photographs, represent less- tlan-fundamental differences. This is illustrated by a coarsely-crystallized specimen from the Las Chispas mine, Mexico. Someareas give the small cell while other, seemingly- ;aentlc.t areas give an intermediate cell (o - 26,b - L5, c - 12). Frondel has reported that-ihe material from this mine gives the double cell. original classification iilo one series,with polybasite as the Sb ) As end-member rnd peardite as the As analogue, is preferable becauseit recognizesthe basic similarity of af potybarite-pearceite mirlrai". -
Mineralogy and Petrology
Title Cervelleite, Ag4TeS: solution and description of the crystal structure Authors Bindi, L; Spry, PG; Stanley, Christopher Date Submitted 2016-03-15 Mineralogy and Petrology Cervelleite, Ag4TeS: solution and description of the crystal structure --Manuscript Draft-- Manuscript Number: MIPE-D-15-00008R1 Full Title: Cervelleite, Ag4TeS: solution and description of the crystal structure Article Type: Standard Article Keywords: cervelleite; Ag-Te-S system; Ag-Cu sulfotellurides; crystal structure; aguilarite; acanthite Corresponding Author: Luca Bindi, Prof University of Florence Florence, ITALY Corresponding Author Secondary Information: Corresponding Author's Institution: University of Florence Corresponding Author's Secondary Institution: First Author: Luca Bindi, Prof First Author Secondary Information: Order of Authors: Luca Bindi, Prof Christopher Stanley Paul G Spry Order of Authors Secondary Information: Funding Information: Abstract: Examination of the type specimen of cervelleite throws new light on its structure demonstrating how earlier researchers erred in describing the mineral as cubic. It was found to be monoclinic, space group P21/n, with a = 4.2696(4), b = 6.9761(5), c = 8.0423(7) Å, β = 100.332(6)°, V = 235.66(3) Å3, Z = 4. The crystal structure [R1 = 0.0329 for 956 reflections with I > 2σ(I)] is topologically identical to that of acanthite, Ag2S, and aguilarite, Ag4SeS. It can be described as a body-centered array of tetrahedrally coordinated X atoms (where X = S and Te) with Ag2X4 polyhedra in planes nearly parallel to (010); the sheets are linked by the other silver position (i.e., Ag1) that exhibits a three-fold coordination. Crystal-chemical features are discussed in relation to other copper and silver sulfides/tellurides, and pure metals. -
New Discoveries of Rare Minerals in Montana Ore
New discoveries of rare Au and Ag minerals in some Montana ore deposits Chris Gammons Geological Engineering, Montana Tech • Butte • McDonald Meadows • Virginia City District • Elkhorn (Boulder) District Butte • Produced over 600 million oz of silver • 2nd in U.S. to Couer d’Alene district ID • Produced roughly 3 million oz of gold • 2nd in Montana to Golden Sunlight Mine Mining Engineering, Web Exclusive 2016 Mineral (group) Formula Guilbert & Ziehen, 1964 This study HYPOGENE Argentite Ag2SXX Pearceite‐polybasite (Ag,Cu)16(As,Sb)2S11 XX Proustite‐pyrargyrite Ag3(As,Sb)S3 XX Stephanite Ag5SbS4 X Andorite PbAgSb3S6 X Stromeyerite AgCuS X X Ag‐tetrahedrite (Ag,Cu)12Sb4S13 XX Furutobeite (Cu,Ag)6PbS4 X Larosite (Cu,Ag)21(Pb,Bi)2S13 X Matildite AgBiS2 X Jalpaite Ag3CuS2 X Electrum AgAu X Petzite Ag3AuTe2 X Hessite Ag2Te X Empressite (?) AgTe X SUPERGENE Acanthite Ag2SXX Silver Ag X X Cerargyrite AgCl X furotobeite: (Cu,Ag)6PbS4 bornite furutobeite bornite stromeyerite + chalcocite furutobeite Mt. Con mine (AMC # 591) larosite: (Cu,Ag)21(Pb,Bi)2S13 stromeyerite larosite wittichenite Cu3BiS3 strom mawsonite Cu6Fe2SnS8 chalcocite pyrite pyrite bornite MT. Con 5933 Occurrences of furutobeite and larosite: Furutobeite Larosite • None in U.S. • None in U.S. • < 5 locations world‐wide • Butte = 3rd (?) locality • Type locality = Furutobe world‐wide mine, Japan (Kuroko‐type VMS) Fred Larose Early prospector in Cobalt silver camp, Ontario jalpaite: Ag3CuS2 Barite Wittichenite Cu3BiS3 Jalpaite Bornite Jalpaite AMC 4756 Anselmo Mine EPMA‐BSE image Goldfieldite Cu10Te 4S13 Bi‐Cu‐Se‐telluride Tennantite or enargite Emplectite: CuBiS2 Bi‐Cu‐Se‐telluride Hessite (Ag2Te) Empressite (AgTe) St. -
Growth of Synthetic Silver Wires from Natural Acanthite Calvin J
Cedarville University DigitalCommons@Cedarville The Research and Scholarship Symposium The 2016 yS mposium Apr 20th, 11:00 AM - 2:00 PM Growth of Synthetic Silver Wires from Natural Acanthite Calvin J. Anderson Cedarville University, [email protected] Follow this and additional works at: http://digitalcommons.cedarville.edu/ research_scholarship_symposium Part of the Geology Commons, and the Mineral Physics Commons Anderson, Calvin J., "Growth of Synthetic Silver Wires from Natural Acanthite" (2016). The Research and Scholarship Symposium. 44. http://digitalcommons.cedarville.edu/research_scholarship_symposium/2016/poster_presentations/44 This Poster is brought to you for free and open access by DigitalCommons@Cedarville, a service of the Centennial Library. It has been accepted for inclusion in The Research and Scholarship Symposium by an authorized administrator of DigitalCommons@Cedarville. For more information, please contact [email protected]. Growth of Synthetic Silver Wires from Natural Acanthite Wire silver is an unusual crystal habit of native silver which is intimately associated with acanthite (Ag2S). These delicate wires have been collected for several centuries, but much remains unknown regarding their growth mechanism and crystal structure. This study has successfully produced synthetic silver wires from natural acanthite in order to investigate the nature of their crystallinity. Chunks of crude acanthite crystals from the Hongda mine, Shanxi Province, China, were trimmed into roughly 1 cm chunks for growth experiments. Preexisting silver wires, which appeared to be natural, were avoided. Several techniques were explored with varying degrees of success. Attempts using a benchtop furnace failed to produce any wires. However, a silver film, which formed on the acanthite surface, confirmed that decomposition of the sulfide indeed occurs in excess of 450°C. -
On the Symmetry and Crystal Structure of Aguilarite, Ag4ses
Mineralogical Magazine, February 2013, Vol. 77(1), pp. 21–31 On the symmetry and crystal structure of aguilarite, Ag4SeS 1,2, 3 L. BINDI * AND N. E. PINGITORE 1 Dipartimento di Scienze della Terra, Universita`degli Studi di Firenze, Via G. La Pira 4, I-50121 Firenze, Italy 2 CNR À Istituto di Geoscienze e Georisorse, Sezione di Firenze, Via G. La Pira 4, I-50121 Firenze, Italy 3 Department of Geological Sciences, The University of Texas at El Paso, El Paso, TX-79968-0555 Texas, USA [Received 10 December 2012; Accepted 9 January 2013; Associate Editor: Giancarlo Della Ventura] ABSTRACT An examination of a specimen of aguilarite from the type locality provides new data on the chemistry and structure of this mineral. The chemical formula of the crystal used for the structural study is (Ag3.98Cu0.02)(Se0.98S0.84Te0.18), on the basis of 6 atoms. The mineral was found to be monoclinic, ˚ crystallizing in space group P21/n, with a = 4.2478(2), b = 6.9432(3), c = 8.0042(5) A, b = 100.103(2)º, ˚ 3 V = 232.41(2) A and Z = 4. The crystal structure [refined to R1 = 0.0139 for 958 reflections with I >2s(I)] is topologically identical to that of acanthite, Ag2S. It can be described as a body-centred array of tetrahedrally coordinated X atoms (X = S, Se and Te) with Ag2X3 triangles in planes nearly parallel to (010); the sheets are linked by the Ag1 silver site, which has twofold coordination. Aguilarite is definitively proved to be isostructural with acanthite; it does not have a naumannite-like structure, as previously supposed.