Carrollite Leaching in H2SO4-Naclo3 Media At
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SAMPLING for COBALT at BORNITE, ALASKA Ry Jeffrey Y
SAMPLING FOR COBALT AT BORNITE, ALASKA Ry Jeffrey Y. Foley %*9 * * * * * * * * * * * * * * * * * * * * * Field Report - January, l9R 11. S. nEPARTMENT OF THE INTERIOR James S. Watt, Secretary BuREAuA OF MINES TARLE OF CONTENTS Page Introduction ................................................ Economic Geoloqy............................................ Work by the Bureau.......................................... Recommendations............................................. References ................................................. SAMDLING FOR cnRALT AT RORNITE, ALASKA By Jeffrey Y. Foley 1 INTRODIICTION Carrollite (CuCo2S4), an ore mineral of cobalt, is known to occur in the Ruby Creek Cu-Zn deposit at Bornite (fig. 1), in northwest Alaska (5, q). 2 The events leading to mineralization of dolomite and argillite units and the distribution of these rocks in the Bornite district are among the topics covered in a PhD discertation by M. W. Hitzman of Stan- ford University (in progress). Hitzman has identified carkollite and cobaltiferous pyrite at numerous intersections in diamond drill core belonging to Rear Creek Mining Corporation, the present operator of the property. A brief visit to collect bulk samples was made by a Bureau geologist in July, 19R1, as part of the Alaska Critical Metals program. ECONOMIC GEOLOGY Hitzman summarizes the distribution of cobalt as occurring: 1) "...as late cobaltiferous pyrite rims on earlier formed pyrite grains in pyritiferous, ferroan dolo- mite with disseminated sphalerite and massive siderite" 2) "...as carrollite in high-grade hornite, chalcocite, chalcopyrite, and sphalerite ore at higher levels in the deposit." 1 Geologist, U.S. Rureau of Mines, Alaska Field Operations Center, Fairbanks. 2 Underlined numbers in parentheses refer to items in the list of references at the end oF this report. ; - > . ; - .>;. -1,; g n/ /- ; > @ ! - xi #."R-: 3 2 vl- t 7:'i "^. -
DESCRIPTIVE MODEL of KIPUSHI Cu-Pb-Zn
Model 32c DESCRIPTIVE MODEL OF KIPUSHI Cu-Pb-Zn By Dennis P. Cox and Lawrence R. Bernstein DESCRIPTION Massive base-metal sulfides and As-sulfosalts in dolomite breccias characterized by minor Co, Ge, Ga, U, and V. GEOLOGICAL ENVIRONMENT Rock Types Dolomite, shale. No rocks of unequivocal igneous origin are related to ore formation. [The pseudoaplite at Tsumeb is herein assumed to be a metasedimentary rock following H. D. LeRoex (1955, unpublished report).] Textures Fine-grained massive and carbonaceous, laminated, stromatolitic dolomites. Age Range Unknown; host rocks are Proterozoic in Africa, Devonian in Alaska, Pennsylvanian in Utah. Depositional Environment High fluid flow along tabular or pipe-like fault- or karst (?)-breccia zones. Tectonic Setting(s) Continental platform or shelf terrane with continental or passive margin rifting. Ore formation at Tsumeb and Ruby Creek predates folding. Associated Deposit Types Sedimentary copper, U-veins, barite veins. Sedimentary exhalative Pb-Zn may be a lateral facies. DEPOSIT DESCRIPTION Mineralogy Ruby Creek: pyrite, bornite, chalcocite, chalcopyrite, carrollite, sphalerite, tennantite. Tsumeb: galena, sphalerite, bornite, tennantite, enargite. Kipushi: sphalerite, bornite, chalcopyrite, carrollite, chalcocite, tennantite, pyrite. Less abundant minerals in these deposits are linnaeite, Co-pyrite, germanite, renierite, gallite, tungstenite, molybdenite, and native Bi. Bituminous matter in vugs. At Apex mine, marcasite. Texture/Structure Massive replacement, breccia filling, or stockwork. Replacement textures of pyrite after marcasite at Ruby Creek and Apex. Alteration Dolomitization, sideritization, and silicification may be related to mineralization. Early pyrite or arsenopyrite as breccia filling or dissemination. Ore Controls Abundant diagenetic pyrite or other source of S acts as precipitant of base metals in zones of high porosity and fluid flow. -
Cobalt Mineral Ecology
American Mineralogist, Volume 102, pages 108–116, 2017 Cobalt mineral ecology ROBERT M. HAZEN1,*, GRETHE HYSTAD2, JOSHUA J. GOLDEN3, DANIEL R. HUMMER1, CHAO LIU1, ROBERT T. DOWNS3, SHAUNNA M. MORRISON3, JOLYON RALPH4, AND EDWARD S. GREW5 1Geophysical Laboratory, Carnegie Institution, 5251 Broad Branch Road NW, Washington, D.C. 20015, U.S.A. 2Department of Mathematics, Computer Science, and Statistics, Purdue University Northwest, Hammond, Indiana 46323, U.S.A. 3Department of Geosciences, University of Arizona, 1040 East 4th Street, Tucson, Arizona 85721-0077, U.S.A. 4Mindat.org, 128 Mullards Close, Mitcham, Surrey CR4 4FD, U.K. 5School of Earth and Climate Sciences, University of Maine, Orono, Maine 04469, U.S.A. ABSTRACT Minerals containing cobalt as an essential element display systematic trends in their diversity and distribution. We employ data for 66 approved Co mineral species (as tabulated by the official mineral list of the International Mineralogical Association, http://rruff.info/ima, as of 1 March 2016), represent- ing 3554 mineral species-locality pairs (www.mindat.org and other sources, as of 1 March 2016). We find that cobalt-containing mineral species, for which 20% are known at only one locality and more than half are known from five or fewer localities, conform to a Large Number of Rare Events (LNRE) distribution. Our model predicts that at least 81 Co minerals exist in Earth’s crust today, indicating that at least 15 species have yet to be discovered—a minimum estimate because it assumes that new minerals will be found only using the same methods as in the past. Numerous additional cobalt miner- als likely await discovery using micro-analytical methods. -
Cobalt—For Strength and Color
USGS Mineral Resources Program Cobalt—For Strength and Color Cobalt is a shiny, gray, brittle metal that is best known for creating an intense blue color in glass As part of a broad mission to and paints. It is frequently used in the manufacture of rechargeable batteries and to create alloys that conduct research and provide maintain their strength at high temperatures. It is also one of the essential trace elements (or “micro information on nonfuel mineral nutrients”) that humans and many other living creatures require for good health. Cobalt is an important resources, the U.S. Geological component in many aerospace, defense, and medical applications and is a key element in many clean Survey (USGS) supports science energy technologies. to understand The name cobalt comes from the German word kobold, meaning goblin. It was given this name by medieval miners who believed that troublesome goblins replaced the valuable metals in their ore with • How and where cobalt a substance that emitted poisonous fumes when smelted. The Swedish chemist Georg Brandt isolated resources form and metallic cobalt—the first new metal to be discovered since ancient times—in about 1735 and identified concentrate in the some of its valuable properties. Earth’s crust • How cobalt resources How Do We Use Cobalt? interact with the environment to affect human and Cobalt has been used to create vivid blue colors ecosystem health in glass and ceramics for thousands of years and it is still an important pigment. Many other uses for • Trends in the supply of cobalt have been developed during the past century. -
Article Benefited from Construc- Ering the Co Dominance Among the Non-Cu Metal Atoms, Tive Reviews by Jochen Schlüter and Taras Panikorovskii
Eur. J. Mineral., 32, 637–644, 2020 https://doi.org/10.5194/ejm-32-637-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Gobelinite, the Co analogue of ktenasite from Cap Garonne, France, and Eisenzecher Zug, Germany Stuart J. Mills1, Uwe Kolitsch2,3, Georges Favreau4, William D. Birch1, Valérie Galea-Clolus5, and Johannes Markus Henrich6 1Geosciences, Museums Victoria, GPO Box 666, Melbourne, Victoria 3001, Australia 2Mineralogisch-Petrographische Abt., Naturhistorisches Museum, Burgring 7, 1010 Vienna, Austria 3Institut für Mineralogie und Kristallographie, Universität Wien, Althanstraße 14, 1090 Vienna, Austria 4independent researcher: 421 Avenue Jean Monnet, 13090 Aix-en-Provence, France 5independent researcher: 10 rue Combe Noire, 83210 Solliès-Toucas, France 6independent researcher: Im Großen Garten 3, 57548 Kirchen (Sieg), Germany Correspondence: Stuart J. Mills ([email protected]) Received: 13 April 2020 – Revised: 30 October 2020 – Accepted: 9 November 2020 – Published: 25 November 2020 Abstract. The new mineral gobelinite, ideally CoCu4.SO4/2.OH/6 6H2O, is a new member of the ktenasite group and the Co analogue of ktenasite, ZnCu4.SO4/2.OH/6 6H2O.q It occurs at Cap Garonne (CG), Var, France (type locality), and Eisenzecher Zug (EZ), Siegerland, Northq Rhine-Westphalia, Germany (cotype lo- cality). The mineral forms pale green, bluish green or greyish green, blocky to thin, lath-like crystals. They are transparent and non-fluorescent, with a vitreous, sometimes also pearly, lustre and a white streak having a pale-green cast. Mohs hardness is about 2.5. The crystals are brittle with an irregular fracture; no cleav- age was observed. -
Sediment-Hosted Copper Deposits of the World: Deposit Models and Database
Sediment-Hosted Copper Deposits of the World: Deposit Models and Database By Dennis P. Cox1, David A. Lindsey2 Donald A. Singer1, Barry C. Moring1, and Michael F. Diggles1 Including: Descriptive Model of Sediment-Hosted Cu 30b.1 by Dennis P. Cox1 Grade and Tonnage Model of Sediment-Hosted Cu by Dennis P. Cox1 and Donald A. Singer1 Descriptive Model of Reduced-Facies Cu 30b.2 By Dennis P. Cox1 Grade and Tonnage Model of Reduced Facies Cu by Dennis P. Cox1 and Donald A. Singer1 Descriptive Model of Redbed Cu 30b.3, by David A. Lindsey2 and Dennis P. Cox1 Grade and Tonnage Model of Redbed Cu by Dennis P. Cox1 and Donald A. Singer1 Descriptive Model of Revett Cu 30b.4, by Dennis P. Cox1 Grade and Tonnage Model of Revett Cu by Dennis P. Cox1 and Donald A. Singer1 Open-File Report 03-107 Version 1.3 2003, revised 2007 Available online at http://pubs.usgs.gov/of/2003/of03-107/ Any use of trade, product or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY 1 345 Middlefield Road, Menlo Park, CA 94025 2 Box 25046, Denver Federal Center, Denver, CO 80225 Introduction This publication contains four descriptive models and four grade-tonnage models for sediment hosted copper deposits. Descriptive models are useful in exploration planning and resource assessment because they enable the user to identify deposits in the field and to identify areas on geologic and geophysical maps where deposits could occur. -
USGS Open-File Report 03-107, V. 1.3, Database Record Pages
DepositID 1 Cont AF NameDeposit Mehirize OtherNames Includes Country Code ALGR Algeria StateProvince Lat.Deg 33 Long.Deg 0 Dec.Lat 33.8472222 Lat.Min 50 Long.Min -20 Dec.Long -.341666667 Lat.Sec 50 Long.Sec -30 OreMmt CuGrade% CoGrade% AgGradeppm CuMmt Subtype Redbed Cu Age Cretaceous, Lower Aptian Ma 115 Unit HostRocks Green argillite, sandstone HangingwallBeds FootwallRocks Conglomerate Mineralogy Chalcocite, malachite TraceMinerals Comments Reference Caia, J. 1976, Paleogeographical and sedimentological controls of copper, lead, and zinc mineralization in the Lower Cretaceous sandstones of Africa: Economic Geology, V. 71, p. 409-422 DepositID 2 Cont AF NameDeposit Tansrift OtherNames Tamarift Includes Country Code MRCO Morocco StateProvince Lat.Deg 33 Long.Deg -4 Dec.Lat 33 Lat.Min 0 Long.Min -15 Dec.Long -4.25 Lat.Sec 0 Long.Sec 0 OreMmt 1 CuGrade%1.3 CoGrade% AgGradeppm CuMmt .013 Subtype Redbed Cu Age Cretaceous Ma 120 Unit HostRocks Red sandstone HangingwallBeds FootwallRocks Mineralogy TraceMinerals Comments Reference Caia, J. 1976, Paleogeographical and sedimentological controls of copper, lead, and zinc mineralization in the Lower Cretaceous sandstones of Africa: Economic Geology, V. 71, p. 409-422. Habashi F. and Bassyouni, F.A., 1982, Mineral resources of the Arab countries: Quebec, Chemecon Publishing Ltd.,Laval Univ., 2nd Edition.112 p. Kirkham, R.V, Carriere, J.J., Laramee, R.M., and Garson, D.F., 1994, Global distribution of sediment-hosted stratiform copper deposits and occurrences: Geological Survey of Canada Open File 2915b, 256 p. DepositID 3 Cont AF NameDeposit Tiloula OtherNames Includes Country Code ALGR Algeria StateProvince Lat.Deg 32 Long.Deg 0 Dec.Lat 32.85 Lat.Min 51 Long.Min -27 Dec.Long -.45 Lat.Sec 0 Long.Sec 0 OreMmt CuGrade% CoGrade% AgGradeppm CuMmt Subtype Redbed Cu Age Cretaceous, L.Aptian Ma 115 Unit HostRocks Green argillite, sandstone HangingwallBeds FootwallRocks Conglomerate Mineralogy Chalcocite, malachite TraceMinerals Comments Reference Caia, J. -
Spatial Distribution of the Ophiolite-Hosted Co–Ni–As-Rich Hydrothermal Mineralization in the Punta Corna Mining Complex, Lanzo Valleys, Northern Italy
EGU21-7589 https://doi.org/10.5194/egusphere-egu21-7589 EGU General Assembly 2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Spatial distribution of the ophiolite-hosted Co–Ni–As-rich hydrothermal mineralization in the Punta Corna Mining complex, Lanzo Valleys, Northern Italy Giovanni Grieco1, Marilena Moroni1, Micol Bussolesi2, Alessandro Cavallo2, and Simone Orizio1 1Earth Science Department, University of Milan, via S. Botticelli 23, 20133, Milan, Italy 2Department of Earth and Environmental Sciences – DISAT, University of Milan-Bicocca, p.zza della Scienza 1–4, 2016 Milan, Italy Cobalt is a transition metal with a trace element abundance in the Earth’s crust (26.6 ppm). It forms mainly sulfides like carrollite, siegenite and linneite and enters the cobaltite-gersdorffite solid solution and di-tri-arsenides safflorite, rammelsbergite and skutterudite while erythrite and asbolane are secondary Co phases. Cobalt is a Critical Raw Material for the EU, strategically important due to its use in the industry (batteries, superalloys, catalysts etc.). Italy hosts several Co-bearing hydrothermal deposits, which were variably exploited in the past. In this work we focus on the Co-Fe-Ni hydrothermal veins emplaced within the metabasites of the Lanzo Valleys ophiolite complex in the western sector of the Alpine belt. The vein system is collectively called “Punta Corna mining complex”, and was exploited for Fe, Ag and later Co in the past (Castelli et al., 2011, Moroni et al., 2019). A detailed field survey of the past cobalt mining works was carried out in summer 2019, followed by sampling, mostly inside mining tunnels and from waste dumps in order to increase data about this poorly known vein system. -
Paragenesis of Cobalt and Nickel at the Black Butte Copper Project, Meagher County, Montana
PARAGENESIS OF COBALT AND NICKEL AT THE BLACK BUTTE COPPER PROJECT, MEAGHER COUNTY, MONTANA by Joshua White A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geosciences Geology Option Montana Tech of The University of Montana 2012 ii Abstract The Black Butte Copper Project (formerly known as the Sheep Creek deposit) is a sediment hosted, laterally extensive massive sulfide deposit hosted in the mid-Proterozoic Newland Formation in Central Montana. Formation of the deposit occurred during two stages of mineralization: Stage I occurred during deposition of sediment in the Helena Embayment, and Stage II occurred post-deposition. Stage I mineralization is characterized by a large quantity of porous pyrite hosting significant Co/Ni/As mineralization in the form of both ion substitution within the pyrite chemical lattice and small (< 1 μm) mineral inclusions of Ni-rich alloclasite. Stage II mineralization reworked the existing Co/Ni/As mineralization, removing the metals from the pyrite and reprecipitating them as distinct siegenite ((Co,Ni)3S4) and tennantite (Cu12As4S13) grains, usually adjacent to one another. Stage II introduced minor, if any, additional Co/Ni/As mineralization into the deposit. Although siegenite is abundant in Co-rich portions of the ore body and is readily identifiable in hand specimen and under the microscope, stoichiometric relationships based on drill-core assay data suggest that Co and Ni were originally introduced into the deposit in the form of alloclasite. Although many of the characteristics of SEDEX type deposits are present at Black Butte (e.g., low temperature of formation, laterally extensive massive sulfide horizons, interbedded black shales, abundant barite and local phosphate horizons, hosted within a continental rift) the lack of economic Pb and Zn mineralization in the central ore body and the abundance of Cu/Co/Ni is more typical of red-bed copper deposits. -
Mineralogy of Sulfides
This is a repository copy of Mineralogy of sulfides. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/113362/ Version: Published Version Article: Vaughan, D.J. and Corkhill, C.L. orcid.org/0000-0002-7488-3219 (2017) Mineralogy of sulfides. Elements , 13 (2). pp. 81-87. ISSN 1811-5209 https://doi.org/10.2113/gselements.13.2.81 Reuse This article is distributed under the terms of the Creative Commons Attribution (CC BY) licence. This licence allows you to distribute, remix, tweak, and build upon the work, even commercially, as long as you credit the authors for the original work. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Mineralogy of Sulfides David J. Vaughan1 and Claire L. Corkhill2 1811-5209/17/0013-0081$2.50 DOI: 10.2113/gselements.13.2.81 etal sulfides are the most important group of ore minerals. Here, we The literature on sulfide minerals review what is known about their compositions, crystal structures, is extensive, with a number of overview textbooks and Mphase relations and parageneses. Much less is known about their monographs. Comprehensive surface chemistry, their biogeochemistry, or the formation and behaviour of reviews can be found in Ribbe ‘nanoparticle’ sulfides, whether formed abiotically or biogenically. -
Geology and Sulfide Mineralogy of the Number One Orebody, Ruby Creek Copper Deposit, Alaska
EconomicGeology Vol. 81, 1986, pp. 1675-1689 Geology and Sulfide Mineralogy of the Number One Orebody, Ruby Creek Copper Deposit, Alaska LAWRENCE R. BERNSTEIN* AND DENNIS P. COX U.S. GeologicalSurvey, 345 MiddlefieldRoad, Mail Stop984, MenloPark, California94025 Abstract The Number One orebodyis the largestand mostsulfide-rich ore zone (at least 200,000 tonscontaining 8.4 wt % Cu) at the Ruby Creek copperdeposit, in the southwesternBrooks Rangeof Alaska.Pyrite and copper-bearing sulfide minerals are concentratedwithin the matrix of a dolostonebreccia body, which is enclosedby phyllite andcalcic marble of Middle to Late Devonianage. The Number One orebodyhas three mineralogicalzones that gradeinto each other: (1) an outer zone,widest toward the hangingwall, containingmostly pyrite with minor amountsof chalcopyriteand traces of carrollitcand sphalerite;(2) an intermediatezone con- tainingmajor chalcopyriteand pyrite, minor tennantite-tetrahedrite,bornitc, carrollitc, and sphalerite,and tracesof galena;and (3) a core zone containingmajor bornitc, chalcopyrite, pyrite, and chalcocite,minor carrollitc, digenite, and sphalerite,and tracesof galena,covellite, and the germanium-bearingsulfides renierite and germanitc.Small clots of anthracitelike organicmaterial (anthraxolite) are foundthroughout the ore. Muchof the pyrite is fine grained andwas deposited before the othersulfides, being increasingly replaced by Cu-bearingsulfides from the outer zoneto the core. Someof thispyrite recrystallizedinto coarsergrains having cobaltiferousrims, and these -
Cobalt—Styles of Deposits and the Search for Primary Deposits
Cobalt—Styles of Deposits and the Search for Primary Deposits By Murray W. Hitzman, Arthur A. Bookstrom, John F. Slack, and Michael L. Zientek Open-File Report 2017–1155 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. Geological Survey William H. Werkheiser, Deputy Director exercising the authority of the Director U.S. Geological Survey, Reston, Virginia: 2017 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 https://www.usgs.gov/ or call 1–888–ASK–USGS (1–888–275–8747). For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Hitzman, M.W., Bookstrom, A.A., Slack, J.F., and Zientek, M.L., 2017, Cobalt—Styles of deposits and the search for primary deposits: U.S. Geological Survey Open-File Report 2017–1155, 47 p., https://doi.org/10.3133/ofr20171155. ISSN 2331-1258 (online) Contents Slide Presentation ........................................................................................................................................