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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. -
Supergene Mineralisation of the Boyongan Porphyry Copper-Gold Deposit, Surigao Del Norte, Philippines
Supergene Mineralisation of the Boyongan Porphyry Copper-Gold Deposit, Surigao del Norte, Philippines by Allan Maglaya Ignacio B.Sc. Geology, National Institute of Geological Sciences University of the Philippines Thesis submitted in partial fulfilment of the requirements of the Masters of Economic Geology Degree Centre for Ore Deposit Research, University of Tasmania December, 2005 DECLARATION OF ORIGINALITY This thesis contains no material which has been accepted for a degree of diploma by the University of Tasmania or any other institution, except by way of background information and duly acknowledged in the thesis, and contains no previous material previously pub- lished or written by another person except where due acknowledgement is given. Allan Maglaya Ignacio 01 December 2005 _________________________ STATEMENT OF AUTHORITY OF ACCESS This thesis may not to be made available for loan or copying for 1.5 years following the date this statement was signed. Following that time, the thesis may be available for loan and lim- ited copying in accordance with Copyright Act 1968. Allan Maglaya Ignacio 01 December 2005 _________________________ TABLE OF CONTENTS Page (s) LIST OF FIGURES …………………………………………………….. i - iii LIST OF APPENDICES ………………………………………………… iv ACKNOWLEDGMENTS ………………………………………………. v ABSTRACT ……………………………………………………………... vi - vii 1.0 INTRODUCTION ………………………………………………………. 1 - 8 1.1 Introduction …………………………………………………………. 1 1.2 Aims and Objectives ……………………………………………….. 1 1.3 Methods Employed …………………………………………………. 2 1.4 Location and Accessibility …………………………………………. 3 1.5 Climate ……………………………………………………………... 5 1.6 Previous Work ……………………………………………………… 5 2.0 GEOLOGICAL SETTING ………………………………………………. 9 - 37 2.1 Introduction ………………………………………………………. 9 2.2 Regional Tectonics …………….…………………………………. 9 2.3 Regional and Local Stratigraphy ………………………………... 11 2.3.1 Basement (Cretaceous-Paleogene) ………………………. 11 2.3.2 Bacuag Formation (Oliogocene-Miocene) .…………….. -
The Mineral Industry of Peru in 1999
THE MINERAL INDUSTRY OF PERU By Alfredo C. Gurmendi With a population of more than 27 million, Peru had a gross concessions for construction and operation of public domestic product (GDP) of $52 billion,1 or $116 billion in terms infrastructure (roads, ports, and airports), and embarked on of purchasing power parity in 1999 (Ministerio de Energía y fiscal austerity and investment in social development and Minas, 1999a, p. 1; U.S. Central Intelligence Agency, 2000). agriculture (Ministerio de Energía y Minas, 1999c, p. 3, 6). The GDP grew by 3.8%, which was considerably higher than The Asian Pacific Economic Council’s (APEC) 18 members, 0.7% in 1998, and the average inflation rate for the year was which included Peru, had a GDP of $13 trillion, which 3.7%, which was lower than 6.0% in 1998. Minerals and represented 56% of world income and 46% of global trade in hydrocarbon industries were 11.8% of Peru’s 1999 GDP. 1999. APEC was expected to provide increased opportunities Mining export revenues represented 49.2% of total exports of to Peru to expand and diversify its international trade $6.1 billion, the trade deficit was about $0.6 billion. In spite of (Ministerio de Energía y Minas, 1999c, p. 8). the effects of El Niño, the Asian financial crisis, the instability CONITE reported that since 1993, Peru has received $15.7 in the Brazilian markets of Rio de Janeiro and São Paulo, and billion of direct foreign investments and $12.4 billion of the lower prices for its major mineral exports (mainly copper, committed new foreign investments. -
2018 Resource and Reserves
Resources & Reserves as at 31 December 2018 Contents Page number About this report 2 Definitions 4 Metals and Minerals: Copper 5 Zinc 17 Nickel 34 Ferroalloys 38 Aluminium/Alumina 42 Iron ore 43 Energy Products: Coal 47 Oil 66 About this report We report our resources and reserves in accordance with the 2012 edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (JORC Code), the 2016 edition of the South African Code for Reporting of Mineral Resources and Mineral Reserves (SAMREC), the Canadian Institute of Mining, Metallurgy and Petroleum (CIM) Standards on Mineral Resources and Reserves (2014 edition) and the Petroleum Resources Management System (PRMS) for reporting oil and natural gas Reserves and Resources. Overview Nickel The resource and reserve data in the following tables are The Canadian and New Caledonian Mineral Resources as at 31 December 2018, unless otherwise noted. For and Mineral Reserves estimates are prepared in comparison purposes, data for 2017 has been included. accordance with the CIM Definition Standards on Mineral Resources and Mineral Reserves, adopted by CIM Council Metric units are used throughout. on 10 May 2014, and the CIM Estimation of Mineral Resources and Mineral Reserves Best Practice Guidelines, All data is presented on a 100% asset basis, with the adopted by CIM Council on 23 November 2003, and have Glencore attributable percentage shown against each been compiled using geo-statistical and/or classical asset, with the exception of Oil assets which are shown on methods, plus economic and mining parameters a working interest basis. appropriate to each project. -
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. -
Ivanhoe Mines Discovers Potentially Significant Iron Oxide Copper/Gold Mineralization at Australian Cloncurry Project
March 21, 2005 Ivanhoe Mines Discovers Potentially Significant Iron Oxide Copper/Gold Mineralization at Australian Cloncurry Project BRISBANE, AUSTRALIA — Douglas Kirwin, Ivanhoe Mines’ Executive Vice-President, Exploration, announced today that the company has discovered a new deposit of potentially significant, iron oxide copper-gold (IOCG) mineralization at its Cloncurry Project, approximately 160 kilometres southeast of Mount Isa, in northwestern Queensland, Australia. Ivanhoe’s geologists believe that the discovery is geologically similar to the Proterozoic IOCG, breccia-hosted deposits at the Olympic Dam, Prominent Hill and Ernest Henry mines, also in Australia. The Cloncurry project is 100%-owned by Ivanhoe Cloncurry Mines Pty. Ltd., a wholly-owned, indirect subsidiary of Ivanhoe Mines Ltd. The new discovery is at the Swan prospect, a 300-metre-wide by 400-metre-long magnetic anomaly located 600 metres southwest of the former Mount Elliott gold and copper mine. Ivanhoe recently completed a preliminary, 1,600-metre, diamond drilling program to test the Swan anomaly. High-grade IOCG, breccia-hosted, supergene and hypogene chalcocite and gold mineralization was encountered in six holes to a depth of at least 350 metres below surface. The mineralization is open-ended along strike and to depth. Hole MEHQ-1069 intersected 79 metres grading 1.45% copper and 0.99 g/t gold (a copper equivalent grade of 2.09%), starting at a depth of 83 metres down hole. Hole MEHQ-1068 encountered 115 metres grading 0.96% copper and 0.86 g/t gold (a copper equivalent grade of 1.52%), commencing at a depth of 65 metres down hole. -
SOUTHERN COPPER CORPORATION (Exact Name of Registrant As Specified in Its Charter)
Table of Contents UNITED STATES SECURITIES AND EXCHANGE COMMISSION Washington, D.C. 20549 FORM 10-K ⌧ ANNUAL REPORT PURSUANT TO SECTION 13 OR 15(d) OF THE SECURITIES EXCHANGE ACT OF 1934 For the fiscal year ended: December 31, 2013 OR TRANSITION REPORT PURSUANT TO SECTION 13 OR 15(d) OF THE SECURITIES EXCHANGE ACT OF 1934 For the transition period from to Commission File Number: 1-14066 SOUTHERN COPPER CORPORATION (Exact name of registrant as specified in its charter) Delaware 13-3849074 (State or other jurisdiction of incorporation or organization) (I.R.S. Employer Identification No.) 1440 East Missouri Avenue Suite 160 Phoenix, AZ 85014 (Address of principal executive offices) (Zip code) Registrant’s telephone number, including area code: (602) 264-1375 Securities registered pursuant to Section 12(b) of the Act: Title of each class: Name of each exchange on which registered: Common stock, par value $0.01 per share New York Stock Exchange Lima Stock Exchange Securities registered pursuant to Section 12(g) of the Act: None Indicate by check mark if the registrant is a well-known seasoned issuer, as defined in Rule 405 of the Securities Act. Yes ⌧ No Indicate by check mark if the registrant is not required to file reports pursuant to Section 13 or Section 15(d) of the Act. Yes No ⌧ Indicate by check mark whether the registrant (1) has filed all reports required to be filed by Section 13 or 15(d) of the Securities Exchange Act of 1934 during the preceding 12 months (or for such shorter period that the registrant was required to file such reports), and (2) has been subject to such filing requirements for the past 90 days Yes ⌧ No Indicate by check mark whether the registrant has submitted electronically and posted on its corporate Website, if any, every Interactive Data File required to be submitted and posted pursuant to Rule 405 of Regulation S-T (§ 232.405 of this chapter) during the preceding 12 months (or for such shorter period that the registrant was required to submit and post such files). -
The Politics of Private Welfare in the Peruvian Mining Industry
Extracting from the Extractors: The Politics of Private Welfare in the Peruvian Mining Industry By Cecilia Perla B.A. Economics, Universidad Católica del Perú, 2001 M.A. Economics of Development, Institute of Social Studies, Holland, 2004 M.A. Political Science, Brown University, 2007 A Dissertation Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in the Department of Political Science at Brown University Providence, Rhode Island May 2012 © Copyright 2012 by Cecilia Perla All Rights Reserved ii This dissertation by Cecilia Perla has been accepted in its present form by the Department of Political Science as satisfying the dissertation requirements for the degree of Doctor of Philosophy Date ____________ ________________________ Pauline Jones Luong, Advisor Date ____________ ________________________ Melani Cammett, Reader Date ____________ ________________________ Patrick Heller, Reader Date ____________ ________________________ Barbara Stallings, Reader Approved by the Graduate Council Date ____________ _____________________________________ Peter M. Weber, Dean of the Graduate School iii Curriculum Vitae Cecilia Perla was born in Lima, Perú on June 4, 1978. She received her B.A. in Economics from Universidad Católica del Perú in 2001. After a few years of working for the public and nonprofit sectors, Cecilia pursued graduate studies at the Institute of Social Studies in The Hague, Holland, earning an MA in Economics of Development in 2004. Later on, she moved to the US to continue her education. During her graduate studies in the Department of Political Science at Brown University, Cecilia presented her work in diverse academic forums such as the Latin American Studies Association Conference, the Political Science Studies Association Conference, the University of Lausanne in Switzerland and King’s College, London. -
UNITED STATES SECURITIES and EXCHANGE COMMISSION Washington, D.C
Table of Contents UNITED STATES SECURITIES AND EXCHANGE COMMISSION Washington, D.C. 20549 FORM 10-K ⌧ ANNUAL REPORT PURSUANT TO SECTION 13 OR 15(d) OF THE SECURITIES EXCHANGE ACT OF 1934 For the fiscal year ended: December 31, 2012 OR TRANSITION REPORT PURSUANT TO SECTION 13 OR 15(d) OF THE SECURITIES EXCHANGE ACT OF 1934 For the transition period from to Commission File Number: 1-14066 SOUTHERN COPPER CORPORATION (Exact name of registrant as specified in its charter) Delaware 13-3849074 (State or other jurisdiction of incorporation or organization) (I.R.S. Employer Identification No.) 1440 East Missouri Avenue Suite 160 Phoenix, AZ 85014 (Address of principal executive offices) (Zip code) Registrant’s telephone number, including area code: (602) 264-1375 Securities registered pursuant to Section 12(b) of the Act: Title of each class: Name of each exchange on which registered: Common stock, par value $0.01 per share New York Stock Exchange Lima Stock Exchange Securities registered pursuant to Section 12(g) of the Act: None Indicate by check mark if the registrant is a well-known seasoned issuer, as defined in Rule 405 of the Securities Act. Yes ⌧ No Indicate by check mark if the registrant is not required to file reports pursuant to Section 13 or Section 15(d) of the Act. Yes No ⌧ Indicate by check mark whether the registrant (1) has filed all reports required to be filed by Section 13 or 15(d) of the Securities Exchange Act of 1934 during the preceding 12 months (or for such shorter period that the registrant was required to file such reports), and (2) has been subject to such filing requirements for the past 90 days Yes ⌧ No Indicate by check mark whether the registrant has submitted electronically and posted on its corporate Website, if any, every Interactive Data File required to be submitted and posted pursuant to Rule 405 of Regulation S-T (§ 232.405 of this chapter) during the preceding 12 months (or for such shorter period that the registrant was required to submit and post such files). -
12. Supergene Ore and Gangue Characteristics
12. Supergene Ore and Gangue Characteristics By Randolph A. Koski 12 of 21 Volcanogenic Massive Sulfide Occurrence Model Scientific Investigations Report 2010–5070–C U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Koski, R.A., 2012, Supergene ore and gangue characteristics in volcanogenic massive sulfide occurrence model: U.S. Geological Survey Scientific Investigations Report 2010–5070 –C, chap. 12, 6 p. 183 Contents Mineralogy and Mineral Assemblages ..................................................................................................185 Paragenesis and Zoning Patterns ...........................................................................................................185 -
UYTENBOGAARDTITE, Ag.Aus2, Ln the BULLFROG MINING
89 Canalian Mineralogist Vol. 31, pp. 89-98 (1993) UYTENBOGAARDTITE,Ag.AuS2, lN THEBULLFROG MINING DISTRICT, NEVADA STEPHENB.CASTOR NevadaBureau of Minesand Geology, University of Nevads.Rem, Nevada 89557, U.S.A. JAMES J: SJOBERG IJ.S.Bureau of Mines,Reno Research Center, 1605 Evans Avenue, Reno, Nevada 89507, U.S.A. ABSTRAc"I The rare mineral uyenbogaardtite,Ag3AuS2, has been identified in specimensfrom two mines in the Bultlrog district of southemNevada. The minesexploit gold-silver vein depositsof the low-sulfur type that arehosted by volcanicrocks of middle Mioceneage. At both mines,uytenbogaardtite occurs in local massesof high-gradeore within shallowly to moderatelydipping systemsof quartz-caxbonateveins emplacedduring late Miocene volcanismand extensionaltectonism. Uytenbogaardtite from the Bullfrog district is chemicallyand structurallyidentical to previouslydescribed synthetic and naturalAg3AuS2. It occursin associationwith two types ofelectrum: relatively coarse,early electrurn,with approximatelyequal molar amountsofgold and silver, andlate gold-rich electrum.It is also associatedwith acanthite,copper-bearing sulfides, and products of oxidationsuch as limonite and chrysocolla.Textural evidenceindicates that the uytenbogaardtitereplaced early electrum,formed contemporane- ously with late electrumand acanthite,and that its depositionmay have overlapped,in part, with that of mineralsformed in an oxidizing environment.Equilibrium relationshipsamong electrum, acanthite, and uytenbogaardtite in specimensfrom theBulllirog district -
The Mineral Industry of Peru in 2015
2015 Minerals Yearbook PERU [ADVANCE RELEASE] U.S. Department of the Interior August 2019 U.S. Geological Survey The Mineral Industry of Peru By Yadira Soto-Viruet In 2015, Peru ranked third among the world’s leading to 195,705 from 174,310 in 2014. Of these 195,705 workers, producers of copper (accounted for 9% of world production), about 18% worked in Arequipa Region; 10% worked in Junin silver (15% of world production), and zinc (11% of world Region; 9% each worked in Apurimac Region and La Libertad production); fourth among the world’s leading producers of Region, respectively; and 7% each worked in Cajamarca Region molybdenum (9% of world production) and lead (6% of world and Lima Region, respectively (Ministerio de Energía y Minas, production); fifth among the world’s leading producers of gold 2016a, p. 117–120). (5% of world production); and sixth among the world’s leading As of December, the country’s foreign direct investment producers of tin (7% of world production). According to the (FDI) inflows amounted to about $7.7 billion compared with Ministerio de Energía y Minas (MEM), in 2015, Peru was Latin $7.6 billion in 2014. The balance of FDI in Peru as contributions America’s leading producer of gold, lead, tin, selenium, and to capital amounted to $24.2 billion in 2015, which was about zinc; and the second-ranked producer of cadmium, copper, the same amount as in 2014, and the mining and petroleum molybdenum, phosphate rock, and silver. The country’s world sectors received about 23% and 3% of that amount, respectively.