Solution Deposition of a Bournonite Cupbsbs3 Semiconductor Thin Film from the Dissolution of Bulk Materials with a Thiol-Amine Sol- Vent Mixture Kristopher M
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Mineralization at Le Pulec, Jersey, Channel Islands; No. 1 Lode
134 SHORT COMMUNICATIONS REFERENCES McKay, W. J. (1975) Woodlawn copper-lead-zinc orebody. Ibid. 701-10. Davis, L. W. (1975) Captains Flat lead-zinc orebody. In Knight, C. L. (ed.). Economic Geology of Australia and Papua New Guinea I. Metals. Melbourne, Australasian [Revised manuscript received 2 June 1981] Institute of Mining and Metallurgy, 691-700. Malone, E. J., Olgers, F., Cucchi, F. G., Nicholas, T., and t~) Copyright the Mineralogical Society Dept. of Geology, University of Wollonoong, New South Wales, Australia F. IVOR ROBERTS [Present address: School of Applied Geology, University of New South Wales, PO Box 1, Kensinoton , NSW 2033, Australia] MINERALOGICAL MAGAZINE, MARCH 1982, VOL. 46, PP. 134-6 Mineralization at Le Pulec, Jersey, Channel Islands; No. 1 Lode THE No. 1 Lode is the westernmost and most Mineralization within the Brioverian sediments extensive of three lead-zinc veins cutting Brioverian sediments at Le Pulec. It was described by Williams Anatase is common within the sediments as 2-10 (1871) as being between 1.5 and 1.8 m in width and pm anhedral grains associated with silicates or 183 m in length, with a trend of 340 ~ and the as 10 x 2 #m laths, parallel to the basal cleavage galena was reported to have a high silver content. of the altered phyllosilicates, particularly musco- Since the investigation of the No. 3 Lode (Ixer and vite. Anatase is also found with hematite laths Stanley, 1980) it has been possible to examine (20x 2 /~m) included in early pyrite grains. A several specimens, collected from the recently re- coarse-grained (600 x 20 pm) generation of anatase discovered No. -
The Nature of Waste Associated with Closed Mines in England and Wales
The nature of waste associated with closed mines in England and Wales Minerals & Waste Programme Open Report OR/10/14 BRITISH GEOLOGICAL SURVEY MINERALS & WASTE PROGRAMME OPEN REPORT OR/10/14 The National Grid and other Ordnance Survey data are used with the permission of the The nature of waste associated Controller of Her Majesty’s Stationery Office. OS Topography © Crown with closed mines in England and Copyright. All rights reserved. BGS 100017897/2010 Wales Keywords Abandoned mine waste facilities; Palumbo-Roe, B and Colman, T England and Wales; mineral deposits; environmental impact; Contributor/editor European Mine Waste Directive. Cameron, D G, Linley, K and Gunn, A G Front cover Graiggoch Mine (SN 7040 7410), Ceredigion, Wales. Bibliographical reference Palumbo-Roe, B and Colman, T with contributions from Cameron, D G, Linley, K and Gunn, A G. 2010. The nature of waste associated with closed mines in England and Wales. British Geological Survey Open Report, OR/10/14. 98pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and the Environment Agency that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is given of the source of the extract. The views and statements expressed in this report are those of the authors alone and do not necessarily represent the views of the Environment Agency. -
Interpretation of Exploration Geochemical Data for the Mount Katmai Quadrangle and Adjacent Parts of the Afognak and Naknek Quadrangles, Alaska
Interpretation of Exploration Geochemical Data for the Mount Katmai Quadrangle and Adjacent Parts of the Afognak and Naknek Quadrangles, Alaska By S.E. Church, J.R. Riehle, and R.J. Goldfarb U.S. GEOLOGICAL SURVEY BULLETIN 2020 Descriptive and interpretive supporting data for the mineral resource assessn~entof this Alaska Mineral Resource Assessnzent Program (AMRAP) study area UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For Sale by U.S. Geological Survey, Map Distribution Box 25286, MS 306, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Library of Congress Cataloging-in-PublieatlonData Church, S.E. Interpretation of exploration geochemical data for the Mount Katmai quadrangle and adjacent parts of the Afognak and Nalrnek quadrangles, Alaska 1 by S.E. Church, J.R. Riehle, and R.J. Goldfarb. p. cm. - (U.S. Geological Survey bulletin ;2020) Includes bibliographical references. Supt. of Docs. no. : 119.3 :2020 1. Mines and mineral resources-Alaska. 2. Mining gedogy- Alaska 3. Geochemical prospecting-Alaska I. Riehle, J.R. 11. Goldfarb, R.J. UI. Title. IV. Series. QE75.B9 no. 2020 [TN24.A4] 557.3 5420 93-2012 [553'.09798] CIP CONTENTS Abstract ............................................................................................................................. Introduction...................................................................................................................... -
New Mineral Names*,†
American Mineralogist, Volume 100, pages 1649–1654, 2015 New Mineral Names*,† DMITRIY I. BELAKOVSKIY1 AND OLIVIER C. GAGNE2 1Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18 korp. 2, Moscow 119071, Russia 2Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada IN THIS ISSUE This New Mineral Names has entries for 10 new minerals, including debattistiite, evdokimovite, ferdowsiite, karpovite, kolskyite, markhininite, protochabournéite, raberite, shulamitite, and vendidaite. DEBATTISTIITE* for 795 unique I > 2σ(I) reflections] corner-sharing As(S,Te)3 A. Guastoni, L. Bindi, and F. Nestola (2012) Debattistiite, pyramids form three-membered distorted rings linked by Ag atoms in triangular or distorted tetrahedral coordination. Certain Ag9Hg0.5As6S12Te2, a new Te-bearing sulfosalt from Len- genbach quarry, Binn valley, Switzerland: description and features of that linkage are similar to those in the structures of crystal structure. Mineralogical Magazine, 76(3), 743–750. trechmannite and minerals of pearceite–polybasite group. Of the seven anion positions, one is almost fully occupied by Te (Te0.93S0.07). The Hg atom is in a nearly perfect linear coordination Debattistiite (IMA 2011-098), ideally Ag9Hg0.5As6S12Te2, is a new mineral discovered in the famous for Pb-Cu-Ag-As-Tl with two Te/S atoms. One of five Ag sites and Hg site, which are bearing sulfosalts Lengenbach quarry in the Binn Valley, Valais, very close (separation 1.137 Å), are partially occupied (50%). Switzerland. Debattistiite has been identified in two specimens Thus there is a statistical distribution (50:50) between Hg(Te,S)2 from zone 1 of the quarry in cavities in dolomitic marble with and AgS2(Te,S)2 polyhedra in the structure. -
ABSTRACTS ACTAS IAGOD 2019 31Ene.Pmd
SALTA, ARGENTINA 28-31 AUGUST 2018 15th Quadrennial International Association on the Genesis of Ore Deposits Symposium SPONSORS PLATINUM SPONSORS GOLD SPONSORS SILVER SPONSORS BRONZE SPONSORS COPPER SPONSORS Co-sponsored by SALTA, ARGENTINA 28-31 AUGUST 2018 15th Quadrennial International Association on the Genesis of Ore Deposits Symposium SYMPOSIUM PROCEEDINGS SCIENTIFIC COMMITTEE CHAIR Lira Raúl – (University of Córdoba – CONICET, Argentina) MEMBERS Bineli-Betsi Thierry – (Botswana International University of Science and Technology) Chang Zhaoshan – (Colorado School of Mines, USA) Cherkasov Sergey – (Vernadsky State Geological Museum of Russian Academy of Sciences) Cook Nigel – (University of Adelaide, Australia) Gozalvez Martín – (Geological and Mining Survey of Argentina) Guido Diego – (CONICET/Austral Gold S.A, Argentina) Lentz David – (University of New Brunswick, Economic Geology Chair) López Luis – (National Atomic Energy Commission, Argentina) Mao Jingwen – (Chinese Academy of Geological Sciences/Hebei GEO University, China) Meinert Larry – (Consultant) Pons Josefina – (IIPG – University of Río Negro – University of Comahue – CONICET, Argentina) Rubinstein Nora – (IGEBa–University of Buenos Aires – CONICET) Sanematsu Kenzo – (Geological Survey of Japan, AIST) Schutesky Della Giustina Maria Emilia – (University of Brasília, Brasil) Tornos Fernando – (Spanish National Research Council – CSIC) Watanabe Yasushi – (Faculty of International Resource Sciences, Akita University, Japan) EDITED BY Daniel Rastelli, Dolores Álvarez, Noelia -
SEG Bratislava, Field Trip Report Location: Mitrovica, Trepca Mining Region, Kosovo in Cooperation with Assoc
SEG Bratislava, Field trip report Location: Mitrovica, Trepca mining region, Kosovo In cooperation with Assoc. Prof. Jaroslav Prseek PhD. (University of Science and Technologyk Kraeow) we have sucessfully organized 4-day field trip dedicated to important deposits in Kosovo. Eight SEG members were involved in this trip led by Tomás Klučiar and Peter Varga. During these four days we have visited Pb-Zn deposits (Stan Tergk Artana and Drazhnje)k and Ni-laterite deposits in Glavica. First day our group travelled 12 hours through Hungaryk Sloveniak Serbia to Kosovok where we have accomodated. On second day our group visited the mine in Trepča region – Stan Tergk located near Stari Trg village in the Trepča valleyk about 8 em east of Kosovsea Mitrovica. This is the central mine of the Trepča complex. Mining at Trepca region is documented since the late Middle Ages. In the 20th centuryk the mine was closed during the Kosovo war of 1998-99. The two smelters were destroyed and the mine completely floodedk after Kosovo war the mine was reopened in 2005. Main deposits of mine is Pb-Zn-Ag searn hosted by recrystallized limestone of Upper Triassic age. The deposit was formed during two distinct mineralization stages: an early prograde closed-system and a later retrograde open-system stage. The prograde mineralisation consists mainly of clinopyroxenesk the retrograde mineralisation comprises ilvaitek magnetitek arsenopyritek pyrrhotitek marcasitek pyritek quartz and various carbonates. The open-system character is related to phreatomagmatic explosion and formation of a breccia. The principal ore minerals were deposited from a moderately saline Ca-Na chloride fluid at around 350°C. -
Silver Enrichment in the San Juan Mountains, Colorado
SILVER ENRICHMENT IN THE SAN JUAN MOUNTAINS, COLORADO. By EDSON S. BASTIN. INTRODUCTION. The following report forms part of a topical study of the enrich ment of silver ores begun by the writer under the auspices of the United States Geological Survey in 1913. Two reports embodying the results obtained at Tonopah, Nev.,1 and at the Comstock lode, Virginia City, Nev.,2 have previously been published. It was recognized in advance that a topical study carried on by a single investigator in many districts must of necessity be less com prehensive than the results gleaned more slowly by many investi gators in the course of regional surveys of the usual types; on the other hand the advances made in the study of a particular topic in one district would aid in the study of the same topic in the next. In particular it was desired to apply methods of microscopic study of polished specimens to the ores of many camps that had been rich silver producers but had not been studied geologically since such methods of study were perfected. If the results here reported appear to be fragmentary and to lack completeness according to the standards of a regional report, it must be remembered that for each district only such information could be used as was readily obtainable in the course of a very brief field visit. The results in so far as they show a primary origin for the silver minerals in many ores appear amply to justify the work in the encouragement which they offer to deep mining, irrespective of more purely scientific results. -
Mineral Reconnaissance Programme Report
Natural Environment Research Council Institute of Geological Sciences Mineral Reconnaissance Programme Report -4 A report prepared for the Department of Industry This report relates to work carried out by the Institute of Geological Sciences on behalf of the Department of Industry. The information contained herein must not be published without reference to the Director, Institute of Geological Sciences. D. Ostle Programme Manager Institute of Geological Sciences Nicker Hill, Keyworth, Nottingham NG12 5GG No. 59 Stratabound arsenic and vein antimony mineralisation in Silurian greywackes at Glendinning, south Scotland INSTITUTE OF GEOLOGICAL SCIENCES Natural Environment Research Council Mineral Reconnaissance Programme Report No. 59 Stratabound arsenic and vein antimony mineralisation in Silurian greywackes at Glendinning, south Scotland ’Geology M. J. Gallagher, PhD, MIMM P. Stone, PhD A. E. S. Kemp, MA M. G. Hills, BSc Geochemistry R. C. Jones, BSc R. T. Smith, MSc, Dip Geochem D. Peachey, BSc, B. P. Vickers Geophysics M. E. Parker, BA K. E. Rollin, BSc Mineraiog y B. R. H. Skilton, BSc 0 Crown copyright 1983 London 1983 A report prepared for the Department of industry Mineral Reconnaissance Programme Reports 38 Geophysical evidence for a concealed eastern extension of the Tanygrisiau microgranite and its 11 A study of the space form of the Cornubian granite possible relationship, to mineralisation batholith and its application to detailed gravity surveys in Cornwall 39 Copper-bearing intrusive rocks at Cairngarroch Bay, south-west Scotland -
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). -
Valid Unnamed Minerals, Update 2012-01
VALID UNNAMED MINERALS, UPDATE 2012-01 IMA Subcommittee on Unnamed Minerals: Jim Ferraiolo*, Jeffrey de Fourestier**, Dorian Smith*** (Chairman) *[email protected] **[email protected] ***[email protected] Users making reference to this compilation should refer to the primary source (Dorian G.W. Smith & Ernest H. Nickel (2007): A System of Codification for Unnamed Minerals: Report of the SubCommittee for Unnamed Minerals of the IMA Commission on New Minerals, Nomenclature and Classification. Canadian Mineralogist v. 45, p.983-1055), and to this website . Additions and changes to the original publication are shown in blue print; deletions are "greyed out and struck through". IMA Code Primary Reference Secondary Comments Reference UM1886-01-OC:HNNa *Bull. Soc. Minéral. 9 , 51 Dana (7th) 2 , 1104 Probably an oxalate but if not is otherwise similar to lecontite UM1892-01-F:CaY *Am. J. Sci. 44 , 386 Dana (7th) 2 , 37 Low analytical total because F not reported; unlike any other known fluoride 3+ UM1910-01-PO:CaFeMg US Geol. Surv. Bull. 419, 1 Am. Mineral. 34 , 513 (Ca,Fe,Mg)Fe 2(PO4)2(OH)2•2H2O; some similarities to mitridatite UM1913-01-AsO:CaCuV *Am. J. Sci. 35 , 441 Dana (7th) 2 , 818 Possibly As-bearing calciovolborthite UM1922-01-O:CuHUV *Izv. Ross. Akad. Nauk [6], 16 , 505 Dana (7th) 2 , 1048 Some similarities to sengierite 3+ UM1926-01-O:HNbTaTiU *Bol. Inst. Brasil Sc., 2 , 56 Dana (7th) 1 , 807 (Y,Er,U,Th,Fe )3(Ti,Nb,Ta)10O26; some similarities to samarskite-(Y) UM1927-01-O:CaTaTiW *Gornyi Zhurn. -
Mercury's Hollows: Chalcogenide Pyro
44th Lunar and Planetary Science Conference (2013) 2840.pdf MERCURY’S HOLLOWS: CHALCOGENIDE PYRO-THERMOKARST ANALOG OF THERMOKARST ON EARTH, MARS, AND TITAN. J.S. Kargel1 1Department of Hydrology and Water Resources, University of Arizona, Tucson, AZ 85721, USA ([email protected]). Introduction/Summary: MESSENGER has ac- quired stunning images of pitted, light-toned or varie- gated light/dark terrains located primarily on many of Mercury’s crater floors (Fig. 1) and on some ejecta blankets. Termed “hollows” by the imaging team, the pits have been described as unique in the Solar System. However, these terrains are geomorphologically simi- lar to some on Mars formed by sublimation of ice-rich permafrost (Fig. 2) and to lowland thermokarst on Earth formed by permafrost thaw; to “swiss cheese” terrain forming by sublimation of frozen CO2 at the Martian South Pole (Fig. 3); and to terrain at Titan’s poles thought to be hydrocarbon thermokarst (Fig. 4). Mercury lacks eolian processes that could erode the pits, and the pits do not possess volcanic characteris- tics. The most plausible explanation for Mercury’s hollows is terrain degradation involving melting or sublimation of heterogeneous chalcogenide and sul- fosalt mineral assemblages. Adapting the term ther- mokarst, I refer to these Mercurian features as pyro- thermokarst; the etymological redundancy distin- guishes the conditions and mineral agents from the ice- related features on Earth and Mars, though some of the physical processes may be similar. Working Hypothesis: Whereas ice has been long suspected and recently was discovered in permanently shadowed craters of Mercury’s polar regions, the hol- lows occur down to the equator, where neither ice nor sulfur is plausible. -
Revision 1 Trace Element Distributions in (Cu)-Pb-Sb Sulfosalts from the Gutaishan Au–Sb Deposit, South China: Implications Fo
1 Revision 1 2 Trace element distributions in (Cu)-Pb-Sb sulfosalts from the Gutaishan Au–Sb 3 deposit, South China: Implications for formation of high-fineness native gold 4 WEI LI1,2, NIGEL J. COOK3, CRISTIANA L. CIOBANU3, GUIQING XIE1,*, BENJAMIN P. 5 WADE4, SARAH E. GILBERT4 6 1Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, 7 Chinese Academy of Geological Sciences, Beijing 100037, China 8 2Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China 9 3School of Chemical Engineering, The University of Adelaide, 5005 S.A., Australia 10 4Adelaide Microscopy, The University of Adelaide, 5005 S.A., Australia 11 ABSTRACT 12 Compositional data, comprising electron probe microanalysis and laser-ablation inductively coupled 13 plasma mass spectrometry (LA-ICP-MS) trace element data are presented for common (Cu)-Pb-Sb 14 sulfosalts (bournonite, jamesonite, tetrahedrite and boulangerite), subordinate semseyite, heteromorphite, 15 robinsonite and (Cu)-Pb-Bi-Sb sulfosalts, and for accompanying base metal sulfides (BMS) in auriferous 16 gold veins from the Gutaishan Au–Sb deposit, southern China. The objectives of the study were to: 17 identify whether these sulfosalts represent overlooked hosts for precious metals and other trace elements 18 of petrogenetic or economic interest; establish partitioning trends among co-existing sulfosalt species 19 and between sulfosalts and BMS; and to seek evidence for a genetic link between the abundance of (Cu)- 20 Pb-Sb sulfosalts and the high-fineness of native gold in the deposit. All (Cu)-Pb-Sb sulfosalts analyzed 21 were found to be remarkably poor hosts for gold and thus do not contribute to the overall mineralogical * Corresponding author E-mail address: [email protected] 1 22 balance for gold.