Metallurgy and Materials

Total Page:16

File Type:pdf, Size:1020Kb

Metallurgy and Materials Peipei Shi et al. Metallurgy andMetalurgia materials e materiais Geochemical assessment of platinum group metals http://dx.doi.org/10.1590/0370-44672019730038 for phytomining Peipei Shi1,3 Abstract https://orcid.org/0000-0003-3399-0154 Marcello Veiga1,4 Phytomining is suggested as a technology to obtain platinum group metals https://orcid.org/0000-0001-9261-738X (PGMs) nanoparticles from plants grown on the mineralized soils or tailings. Sam- Christopher Anderson2,5 ples from North American Palladium (Canada) and gossans from Broken Hill (BH) https://orcid.org/0000-0003-0935-1475 (Australia) were studied to assess the possibility of using these PGM-rich samples as substrates for phytomining. The bioavailability of PGMs was indirectly assessed using 1University of British Columbia, Mining Engineering, geochemical procedures. The selective extractions showed that the highest available Vancouver - British Columbia - Canada. concentration of Pd is 5.38 ppm in BH gossan 1. The extraction of PGMs by ammo- nium acetate, fulvic acid or citrate-dithionite indicates natural availability to plants. 2Massey University, School of Agriculture and The BH gossan 1 was the best of the five studied samples for phytomining of Pd due to Environment, Palmerston North, available Pd concentration (> 2 mg/kg), low Electric Conductivity (< 2dS/m), high CEC Manawatu-Wanganui - New Zealand. (Cation Exchange Capacity) (38.8 meq/100g), and proper pH (6.5). Cu-tolerant plant species should be chosen to grow on BH gossan 1. A criterium for choosing substrates E-mails: [email protected], [email protected], for phytomining of Pd was developed comprising various classical soil parameters plus [email protected] selective extraction procedures. Keywords: phytomining, platinum group metals, bioavailability, plant growth parameters. REM, Int. Eng. J., Ouro Preto, 73(1), 85-91, jan. mar. | 2020 85 Geochemical assessment of platinum group metals for phytomining 1. Introduction The concept of phytomining is an 2015). Parker et al. (2014) reported the first tion is bound to different minerals that are adaptation of the use of an old concept of use of living plants to recover palladium more difficult to be incorporated by plants using plants for prospecting metals (Chaney and the production of catalytically active but this can change gradually by chemical et al., 2018). The phytomining requires palladium nanoparticles with excellent weathering and biological process (Dairy selection of hyperaccumulating plants, as catalytic activity across a range of coupling Soils and Fertiliser Manual, 2013). The well understanding which metals species reactions that produced higher yields than primary determinant of metal uptake by a are bioavailable in the substrate and how commercial Pd catalyst. This process can plant is the bioavailability of the metal in toxic for the plants they are (Kramer, 2019). reduce the number of production steps the soil-plant system, i.e. how easily plants Plant species and methods for phytomining compared to traditional catalyst production can access the metal in a form they re- for platinum group metals (PGMs) involves methods. In automotive industries, for ex- quire. The type and nature of the substrate growing plants on PGM-rich substrates ample, platinum (Pt), along with palladium constituents, pH, organic matter, cation that are capable of selectively incorporating (Pd), and rhodium (Rh) are coated onto exchange capacity and competing ions have these metals into their cellular structures a substrate housed in the exhaust system all been shown to influence PGM bioavail- (Sheoran et al., 2009). Theoretically, the and act as catalysts to convert toxic vehicle ability (Ko et al., 2008; Wilson-Corral et plants can then be harvested and subjected emissions, such as carbon monoxide (CO), al., 2012). As such, the primary interest of to controlled pyrolysis in order to yield a hydrocarbons (HC) and oxides of nitrogen this study was to use geochemical methods, material with stabilized PGM nanoparticles (NOx), to less harmful substances (Saguru such as sequential-selective extractions, to that can later be used in catalytic reactions et al., 2018). In the soil, a small portion of assess the bioavailability of PGMs from (Siddiq, & Husen, 2016, Dodson et al., metals is available to plants as a large por- high grade PGM samples. 2. Materials and methods Samples from two sites were col- (NAP), Canada and from Broken Hill lected: North American Palladium (BH), Australia. 2.1 North American Palladium (NAP) North American Palladium is a plati- of platinum-group minerals occur either are: palladium tellurides > palladium anti- num group metals producer that has oper- interstitially to sulfides in association monides > palladium sulfides > sperrylite ated Lac des Iles (LDI) Mine in northern with gangue minerals such as plagioclase, (platinum arsenide) > gold-silver alloys. Ontario, Canada since 1993. The mine lies amphibole, chlorite, orthopyroxene, and PGM grades show varying degrees of cor- in the southern end of the Lac des Iles, 106 talc, or at sulfide-silicate boundaries. relation with nickel and copper concentra- km northwest of Thunder Bay, Ontario, The relative abundance of PGM-bearing tions (Yu et al., 2010). Feed, concentrate Canada, in an elliptical mafic-ultramafic minerals in the mill feed and concentrates and tailings samples were collected from intrusive complex (NAP, 2018). A majority from recently mined zones on the property the mineral processing plant. 2.2 Broken Hill (BH) The Broken Hill deposit in western by quartz- and garnet-rich host rocks. formation in the Broken Hill District. New South Wales, Australia has one In the upper parts of the mine, many Two types of gossans were selected to of the richest reserves of lead, zinc and of the sulfide minerals were converted be studied (gossan 1 and 2) with no silver in the world. The Broken Hill by weathering into a large suite of ox- visible lithological differences except ore body consists of a series of closely- ide minerals, some of which were first for the fact that gossan 2 seems denser spaced sulfides-rich deposits separated recognized as new minerals from their than gossan 1. 2.3 Analytical procedures Inductively coupled plasma mass samples were analyzed by a Philips XL- exchangeable metals in soil are the most spectrometry (ICP-MS) and inductively 30 scanning electron microscope (SEM) available to plants (Castilho and Rix, coupled plasma atomic emission spectros- equipped with a Bruker Quantax 200 1993). Citrate-dithionite was used by copy (ICP-AES) analyses for whole-rock energy-dispersion X-ray (EDX) micro- Gray et al. (1996) to selectively dissolve chemistry, and Instrumental Neutron analysis system. amorphous and crystalline Hydrous Activation Analysis (INAA) for PGMs The mineral association and bio- Ferric Oxides (HFO) such as limonite (Ir, Os, Pd, Pt, Rh, Ru) and Au were con- availability of PGMs and Au in all and goethite as well as crystalline iron ducted by Acme Analytical Labs Ltd. in samples were investigated by selective oxide like hematite. This work may be Vancouver. The mineralogy was examined extraction methods of samples ground the first trial to use fulvic acid in selective through quantitative X-ray powder dif- below 0.074 mm. Cu and Ni were also extraction of PGMs and Au. It was ex- fractometry (XRD) at the department of analyzed due to their phytotoxicity that pected that this humic substance could Earth, Ocean & Atmospheric Sciences at may limit plant growth. Ammonium ac- provide additional information about the University of British Columbia. etate (NH4C2H3O2) was used to extract the fraction of the metals that would be Due to the high grade of PGMs readily exchangeable metal species (Fer- bioavailable and possibly incorporated in the BH gossan samples only these reira and Veiga, 1995). It is believed that by plants. Reverse aqua regia was used 86 REM, Int. Eng. J., Ouro Preto, 73(1), 85-91, jan. mar. | 2020 Peipei Shi et al. to dissolve sulfides. This is a mixture tion of nitric acid increases dissolution acid provides complexing ligands for Pt of nitric acid and hydrochloric acid in of sulfides (Tessier et al., 1979). When and Pd that are associated with sulfides a molar ratio of 3:1. Higher concentra- sulfides are dissolved, hydrochloric (Colombo et al., 2008). 2.4 First selective extraction scheme Two sequences of selective extrac- twice in a shaker with 50 mL of lab- due was washed and leached twice for tions were employed. The first extraction grade fulvic acid for 5 h, at 500C. 16 h, heated at 500C with 30 ml 65% consisted of the following steps: 3. Dissolution of amorphous and HNO3, 10 mL 30% HCl (inverse aqua- 1. PGM associated with exchange- crystalline HFO and hematite: The resi- regia) and 10 mL H2O2. able cations: 3 g of sample were agitated due from the previous step was washed 5. Residual PGM associated with for 1 h with 50 mL 1 M NH4C2H3O2. and leached twice with 50 mL of other minerals: the final solid residues 2. PGM associated with extract- 0.3 M ammonium citrate and 1 g so- were melted with borate and dissolved able cations extracted by humic sub- dium dithionite for 16 hours, heated with aqua regia. stances: the residue from the previous at 500C. All solutions from each extraction extraction was washed and leached 4. Dissolution of sulfides: the resi- step were analyzed by ICP-MS. 2.5 Second selective extraction scheme The objective of the second extrac- used a citrate-dithionite leaching process above (step 3). After 4 hours, the pulp tion sequence was to remove more ferric as described by Veiga et al., (1991). The was filtered and the solution analyzed for oxides and associated metals from the method leached 3 g of sample ground Pt,Pd and Au. The procedure was repeated gossan samples since the NAP samples below 0.074 in a shaker at 50 oC with a 3 more times to guarantee that all ferric had low ferric oxides.
Recommended publications
  • Podiform Chromite Deposits—Database and Grade and Tonnage Models
    Podiform Chromite Deposits—Database and Grade and Tonnage Models Scientific Investigations Report 2012–5157 U.S. Department of the Interior U.S. Geological Survey COVER View of the abandoned Chrome Concentrating Company mill, opened in 1917, near the No. 5 chromite mine in Del Puerto Canyon, Stanislaus County, California (USGS photograph by Dan Mosier, 1972). Insets show (upper right) specimen of massive chromite ore from the Pillikin mine, El Dorado County, California, and (lower left) specimen showing disseminated layers of chromite in dunite from the No. 5 mine, Stanislaus County, California (USGS photographs by Dan Mosier, 2012). Podiform Chromite Deposits—Database and Grade and Tonnage Models By Dan L. Mosier, Donald A. Singer, Barry C. Moring, and John P. Galloway Scientific Investigations Report 2012-5157 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 This report and any updates to it are available online at: http://pubs.usgs.gov/sir/2012/5157/ 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 Suggested citation: Mosier, D.L., Singer, D.A., Moring, B.C., and Galloway, J.P., 2012, Podiform chromite deposits—database and grade and tonnage models: U.S.
    [Show full text]
  • Chapter 9 Gold-Rich Porphyry Deposits: Descriptive and Genetic Models and Their Role in Exploration and Discovery
    SEG Reviews Vol. 13, 2000, p. 315–345 Chapter 9 Gold-Rich Porphyry Deposits: Descriptive and Genetic Models and Their Role in Exploration and Discovery RICHARD H. SILLITOE 27 West Hill Park, Highgate Village, London N6 6ND, England Abstract Gold-rich porphyry deposits worldwide conform well to a generalized descriptive model. This model incorporates six main facies of hydrothermal alteration and mineralization, which are zoned upward and outward with respect to composite porphyry stocks of cylindrical form atop much larger parent plutons. This intrusive environment and its overlying advanced argillic lithocap span roughly 4 km vertically, an interval over which profound changes in the style and mineralogy of gold and associated copper miner- alization are observed. The model predicts a number of geologic attributes to be expected in association with superior gold-rich porphyry deposits. Most features of the descriptive model are adequately ex- plained by a genetic model that has developed progressively over the last century. This model is domi- nated by the consequences of the release and focused ascent of metalliferous fluid resulting from crys- tallization of the parent pluton. Within the porphyry system, gold- and copper-bearing brine and acidic volatiles interact in a complex manner with the stock, its wall rocks, and ambient meteoric and connate fluids. Although several processes involved in the evolution of gold-rich porphyry deposits remain to be fully clarified, the fundamental issues have been resolved to the satisfaction of most investigators. Explo- ration for gold-rich porphyry deposits worldwide involves geologic, geochemical, and geophysical work but generally employs the descriptive model in an unsophisticated manner and the genetic model hardly at all.
    [Show full text]
  • Platinum Group Minerals in Eastern Brazil GEOLOGY and OCCURRENCES in CHROMITITE and PLACERS
    DOI: 10.1595/147106705X24391 Platinum Group Minerals in Eastern Brazil GEOLOGY AND OCCURRENCES IN CHROMITITE AND PLACERS By Nelson Angeli Department of Petrology and Metallogeny, University of São Paulo State (UNESP), 24-A Avenue, 1515, Rio Claro (SP), 13506-710, Brazil; E-mail: [email protected] Brazil does not have working platinum mines, nor even large reserves of the platinum metals, but there is platinum in Brazil. In this paper, four massifs (mafic/ultramafic complexes) in eastern Brazil, in the states of Minas Gerais and Ceará, where platinum is found will be described. Three of these massifs contain concentrations of platinum group minerals or platinum group elements, and gold, associated with the chromitite rock found there. In the fourth massif, in Minas Gerais State, the platinum group elements are found in alluvial deposits at the Bom Sucesso occurrence. This placer is currently being studied. The platinum group metals occur in specific Rh and Os occur together in minerals in various areas of the world: mainly South Africa, Russia, combinations. This particular PGM distribution Canada and the U.S.A. Geological occurrences of can also form noble metal alloys (7), and minerali- platinum group elements (PGEs) (and sometimes sation has been linked to crystallisation during gold (Au)) are usually associated with Ni-Co-Cu chromite precipitation of hydrothermal origin. sulfide deposits formed in layered igneous intru- In central Brazil there are massifs (Americano sions. The platinum group minerals (PGMs) are do Brasil and Barro Alto) that as yet are little stud- associated with the more mafic parts of the layered ied, and which are thought to contain small PGM magma deposit, and PGEs are found in chromite concentrations.
    [Show full text]
  • Geological Survey
    DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY ISTo. 162 WASHINGTON GOVERNMENT PRINTING OFFICE 1899 UNITED STATES GEOLOGICAL SUEVEY CHAKLES D. WALCOTT, DIRECTOR Olf NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINERALOGY FOR THE YEAR 1898 BY FRED BOUG-HTOISr WEEKS WASHINGTON GOVERNMENT PRINTING OFFICE 1899 CONTENTS, Page. Letter of transmittal.......................................... ........... 7 Introduction................................................................ 9 List of publications examined............................................... 11 Bibliography............................................................... 15 Classified key to the index .................................................. 107 Indiex....................................................................... 113 LETTER OF TRANSMITTAL. DEPARTMENT OF THE INTERIOR, UNITED STATES GEOLOGICAL SURVEY. Washington, D. C., June 30,1899. SIR: I have the honor to transmit herewith the manuscript of a Bibliography and Index o'f North American Geology, Paleontology, Petrology, and Mineralogy for the Year 1898, and to request that it be published as a bulletin of the Survey. Very respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, Director United States Geological Survey. 1 I .... v : BIBLIOGRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINERALOGY FOR THE YEAR 1898. ' By FEED BOUGHTON WEEKS. INTRODUCTION. The method of preparing and arranging the material of the Bibli­ ography and Index for 1898 is similar to that adopted for the previous publications 011 this subject (Bulletins Nos. 130,135,146,149, and 156). Several papers that should have been entered in the previous bulletins are here recorded, and the date of publication is given with each entry. Bibliography. The bibliography consists of full titles of separate papers, classified by authors, an abbreviated reference to the publica­ tion in which the paper is printed, and a brief summary of the con­ tents, each paper being numbered for index reference.
    [Show full text]
  • Origin of Platinum Group Minerals (PGM) Inclusions in Chromite Deposits of the Urals
    minerals Article Origin of Platinum Group Minerals (PGM) Inclusions in Chromite Deposits of the Urals Federica Zaccarini 1,*, Giorgio Garuti 1, Evgeny Pushkarev 2 and Oskar Thalhammer 1 1 Department of Applied Geosciences and Geophysics, University of Leoben, Peter Tunner Str.5, A 8700 Leoben, Austria; [email protected] (G.G.); [email protected] (O.T.) 2 Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of Science, Str. Pochtovy per. 7, 620151 Ekaterinburg, Russia; [email protected] * Correspondence: [email protected]; Tel.: +43-3842-402-6218 Received: 13 August 2018; Accepted: 28 August 2018; Published: 31 August 2018 Abstract: This paper reviews a database of about 1500 published and 1000 unpublished microprobe analyses of platinum-group minerals (PGM) from chromite deposits associated with ophiolites and Alaskan-type complexes of the Urals. Composition, texture, and paragenesis of unaltered PGM enclosed in fresh chromitite of the ophiolites indicate that the PGM formed by a sequence of crystallization events before, during, and probably after primary chromite precipitation. The most important controlling factors are sulfur fugacity and temperature. Laurite and Os–Ir–Ru alloys are pristine liquidus phases crystallized at high temperature and low sulfur fugacity: they were trapped in the chromite as solid particles. Oxygen thermobarometry supports that several chromitites underwent compositional equilibration down to 700 ◦C involving increase of the Fe3/Fe2 ratio. These chromitites contain a great number of PGM including—besides laurite and alloys—erlichmanite, Ir–Ni–sulfides, and Ir–Ru sulfarsenides formed by increasing sulfur fugacity. Correlation with chromite composition suggests that the latest stage of PGM crystallization might have occurred in the subsolidus.
    [Show full text]
  • MINERALOGY and MINERAL CHEMISTRY of NOBLE METAL GRAINS in R CHONDRITES. H. Schulze, Museum Für Naturkunde, Institut Für Mineralogie, Invalidenstr
    Lunar and Planetary Science XXX 1720.pdf MINERALOGY AND MINERAL CHEMISTRY OF NOBLE METAL GRAINS IN R CHONDRITES. H. Schulze, Museum für Naturkunde, Institut für Mineralogie, Invalidenstr. 43, D-10115 Berlin, Germany, hart- [email protected]. Introduction: Rumuruti-chondrites are a group of [1]. Mostly, NM grains can be encountered as mono- chondrites intermediate between ordinary and carbo- mineralic grains, but multiphase assemblages of two naceous chondrites [1]. The characteristic feature of or three phases were found as well. Host phase of most these chondrites is their highly oxidized mineral as- NM grains are sulfides, either intact like in Rumuruti semblage. Equilibrated olivine usually has a fayalite or weathered to Fe-hydroxides in the desert finds. content around ~39 mole-% Fa. There is almost no Also silicates are frequent host phases (mostly olivine free NiFe-metal in these chondrites [1]. As a conse- and plagioclase). Several grains were found in or ad- quence, noble metals form separate phases [1,2,3] jacent to chromite. which otherwise, due to their siderophilic behavior, Mineralogy and mineral chemistry: Table 1 lists certainly would be dissolved in the FeNi metal. De- the NM minerals detected in R chondrites. Summa- spite the occurrence of noble metal minerals the rizing the results for all R chondrites, tetraferroplati- chemistry does not show any enrichment in these ele- num, sperrylite, irarsite, and osmium are the most ments which are CI-like except for very volatile and abundant NM minerals. Gold seems to be a common chalcophile elements which are even lower [4]. Noble phase, too, but was not so frequently observed due to metal grains were described so far from carbonaceous the lower chemical abundance.
    [Show full text]
  • ECONOMIC GEOLOGY RESEARCH INSTITUTE HUGH ALLSOPP LABORATORY University of the Witwatersrand Johannesburg
    2 ECONOMIC GEOLOGY RESEARCH INSTITUTE HUGH ALLSOPP LABORATORY University of the Witwatersrand Johannesburg ! GEOLOGICAL CHARACTERISTICS OF PGE-BEARING LAYERED INTRUSIONS IN SOUTHWEST SICHUAN PROVINCE, CHINA Y.YAO, M.J. VILJOEN, R.P. VILJOEN, A.H. WILSON, H. ZHONG, B.G. LIU, H.L. YING, G.Z. TU and N. LUO ! INFORMATION CIRCULAR No. 358 3 UNIVERSITY OF THE WITWATERSRAND JOHANNESBURG GEOLOGICAL CHARACTERISTICS OF PGE-BEARING LAYERED INTRUSIONS IN SOUTHWEST SICHUAN PROVINCE, CHINA by Y. YAO1, M. J. VILJOEN2, R. P. VILJOEN2, A. H. WILSON3, H. ZHONG1, B. G. LIU4, H. L. YING4, G. Z. TU4 AND Y. N. LUO5, ( 1 Economic Geology Research Institute, School of Geosciences, University of the Witwatersrand, P/Bag 3, WITS 2050, Johannesburg, South Africa; 2 Department of Geology and CAMEG, School of Geosciences, University of the Witwatersrand, P/Bag 3, WITS 2050, Johannesburg, South Africa; 3 Department of Geology and Applied Geology, University of Natal, King George V Avenue, Durban, 4001; 4 Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Qijiahuozhi, Deshengmenwai, Beijing 100029, P.R. China; 5 Geological Exploration Bureau of Sichuan Province, Renminglu, Chengdu 610081, P.R. China) ECONOMIC GEOLOGY RESEARCH UNIT INFORMATION CIRCULAR No. 358 December 2001 4 GEOLOGICAL CHARACTERISTICS OF PGE-BEARING LAYERED INTRUSIONS IN SOUTHWEST SICHUAN PROVINCE, CHINA ABSTRACT A number of platinum-group-element (PGE-bearing), layered, ultramafic-mafic intrusions in the Pan-Xi and Danba areas of the southwest Sichuan Province of China have been investigated. The two study areas are located, respectively, in the central and northern parts of the Kangding Axis on the western margin of the Yangtze Platform, a region geologically distinguished by late- Archaean to late-Proterozoic basement and by stable sedimentary sequences.
    [Show full text]
  • The Post-Magmatic Genesis of Sperrylite from Some Gold Placers in South Part of Krasnoyarsk Region (Russia)
    The Post-Magmatic Genesis of Sperrylite from some Gold Placers in South Part of Krasnoyarsk Region (Russia) G.I.Shvedov1, V.V. Nekos1 and A.M. Uimanov2 1Krasnoyarsk Mining-Geological Company. St.K.Marksa 62, Krasnoyarsk, 660049, Russia 2Mining Company "Tamsiz". St.Artelsky 6, Severo-Yeniseysk, 663280, Russia e-mail: [email protected] Krasnoyarsk Region has been one of the hand, the placers sperrylites from rivers – Karagan main gold-mining provinces of Russia from the last (Eastern Sayan), Rudnaya, Bolshoy Khaylyk, century and up to nowadays. While placer deposits Zolotaya (Western Sayan) are characterized by the being mining they have marked constantly Ir, Ru, Rh unpurities presence. It witnesses for platinum-group minerals with gold in common. In absolutely another native sources. For the the main, they were "platinum" (Fe-Pt compounds) comparison, they show the composition of the and "osmiridium" (Os-Ir-Ru alloys). Receiving and sperrylites from original rocks in some ultramafic- studying heavy concentrates from placer deposits, mafic massifs of Eastern Sayan. we have discovered, that practically all of them The majority of the investigated sperrylitic contained sperrylites somehow, independently of grains from placers contains itself inclusions of the region, or another PGM presence or absence. different ore- and rock-forming minerals. One can One has discovered the mineral in placers of the and should use the mineral compositions for following rivers and creeks: Coloromo, Krasavitza, solving the problem on supposed native sources for Garevka, Lombancha, Danilovsky, Bolshaya PGM. Quartz, pyroxenes, micas, common potash Kuzeyeva (Yenisey Ridge), Karagan, Levaya feldspars, plagioclases, garnets, talc and some Zhaima, Mana, Bolshaya Sinachaga (Eastern others were identified by the composition among Sayan), Rudnaya, Zolotaya, Bolchoy Khaylyk the analyzed mineral inclusions.
    [Show full text]
  • 2010 the Annual Report for the Paleoproterozoic Mineralization Research Group
    PPM Annual Report 2010 The Annual Report for the Paleoproterozoic Mineralization Research Group DEpartmENT OF GEOLOGY UNIVERSITY OF JOHANNESBURG The Annual Report of the Paleoproterozoic Mineralization Research (PPM) Group, compiled and edited by HM Rajesh and Nic Beukes. Layout and design by HM Rajesh and the UJ Graphic Studio. Special thanks/Acknowledgements We wish to extend a special word of thanks to all of our corporate and governmental financial supporters (in alphabetical order): African Rainbow Minerals Anglo American Anglo Coal Anglo Gold Ashanti Anglo Platinum Anglo Research Assmang Assore Coaltech Department of Science and Technology (DST) Lonmin National Research Foundation (NRF) Nkomati Joint Venture Rand Uranium (Gold One) Salt River Resources Ltd Please direct all enquiries and applications for research to: Prof. Nic Beukes or Prof. Fanus Viljoen PPM, Department of Geology University of Johannesburg Auckland Park Kingsway Campus PO Box 524, Auckland Park 2006 Johannesburg, South Africa E-mail: [email protected] or [email protected] Tel: +27 (0) 11 559 4712/4710/4711 Fax: +27 (0) 11 559 4702 http://www.uj.ac.za/geology Cover photo: View of the Bokkeveld (in foreground) and Witteberg strata of the Cape Supergroup at Gamkapoort Dam, Western Cape Province INTRODUCTION The PPM Research Group, formed in 1997 as an informal research group in the Department of Geology, has for the past four years been officially recognized by Management of the University of Johannesburg as one of the Research Centres of Excellence at the University. This meant that PPM received an annual research grant from the University Research Committee to strengthen the group especially with respect to funding salaries of support staff and providing additional bursary support to postgraduates and postdoctoral associates.
    [Show full text]
  • HAZEL M. PRICHARD Department of Earth Sciences, Open University, Milton Keynes, Buekinghamshire, U.K
    Canadian Mineralogist Vol. 26, pp. 979-990 (1988) PLATINUM AND PALLADIUM MINERALS FROM TWO PGE-RICH LOCALITIES IN THE SHETLAND OPHIOLITE COMPLEX HAZEL M. PRICHARD Department of Earth Sciences, Open University, Milton Keynes, Buekinghamshire, U.K. MK7 6AA MAHMUD TARKIAN Mineralogiseh-Petrographisehes Institut, Grindelallee48, 2000 Hamburg 13, West Germany ABSTRACT INTRODUCTION The mineralogy of Pt- and Pd-bearing platinum-group Traditionally, the PGM considered typical of minerals (POM), which form a varied assemblage previ- ously un described from other ophiolite complexes, is ophiolite complexes are Os-, Ir- and Ru-bearing recorded from two localities in the Shetland ophiolite, Scot- (Constantinides et al. 1979, Talkington 1981, land. In order of abundance the minerals include sperry- Prichard et al. 1981, Legendre 1982, Auge 1985) and lite, mertieite or stibiopalladinite, Pt-Pd-Cu-Au alloys, are associated with chromitites. Pt and Pd com- hongshiite, genkinite and potarite. All six platinum-group pounds may be more common; for example, sper- elements (POE) form major components of minerals in the rylite has been described from northern Tibet (Yu Shetland ophiolite complex. The different POM occur in & Chou 1979), and one sperrylite grain has been ten- association with "each other. Textural evidence indicates that tatively identified from the Josephine peridotite Ru- and Os-bearing POM formed early and were followed by Ir, Pd-, Rh- and, finally, Pt-bearing POM. The con- (Stockman & Hlava 1984). Chang et al. (1973) have reported the presence of sperrylite and stibiopal- centration of all six POE could be magmatic, but much of the POE mineralogy, except for laurite in the center of ladinite in ophiolites in northwestern China.
    [Show full text]
  • Mineralogy of Cu-Ni-PGE Ore and Sequence of Events in the Copper Cliff South Mine, Sudbury, Ontario
    Mineralogy of Cu-Ni-PGE ore and Sequence of Events in the Copper Cliff South Mine, Sudbury, Ontario Zsuzsanna Magyarosi, David H. Watkinson, and Peter C. Jones Department of Earth Sciences, Carleton University, 1125 Colonel By Drive, Ottawa, Ontario, Canada K1S 5B6 e-mail: [email protected] The Sudbury Structure is the largest Cu- country rocks are Copper Cliff rhyolite and Ni-PGE producer in the world. It is an impact McKim metasediments. structure in rocks of the Superior Province to the The 800 and 810 ore bodies are the two North and the Southern Province to the South. major deposits in the Copper Cliff South mine, The Sudbury Igneous Complex is subdivided located at the opposite contacts of the quartz into Main Mass and offset dikes (radial and diorite dike with metapelite of McKim concentric): the Main Mass is composed of the Formation. In several places the two ore bodies Contact Sublayer, norite, quartz gabbro and are connected through the center of the dike or granophyre, from bottom to top. The offset there is another ore body parallel to the contact dikes, composed of quartz diorite, intruded along of quartz diorite and country rocks. The primary fracture zones in highly brecciated areas created magmatic minerals in the quartz diorite in by the meteorite impact (Hawley, 1962). The Copper Cliff South include plagioclase, quartz, Copper Cliff Offset, the host of 15 % of the amphibole and biotite. The quartz diorite is sulfide ore (Cochrane, 1984), is one of the radial weakly to strongly altered in the whole area, with offset dikes in the South Range of the Sudbury increasing degree of alteration toward the Structure.
    [Show full text]
  • Sperrylite Saturation in Magmatic Sulfide Melts: Implications for Formation Of
    Revision 3 1 Sperrylite saturation in magmatic sulfide melts: Implications for formation of 2 PGE-bearing arsenides and sulfarsenides 3 Liping Bai 1, Sarah-Jane Barnes 1, Don R. Baker 2 4 5 1 Sciences de la Terre, Université du Québec a Chicoutimi, Québec G7H 2B1, Canada 6 2 Earth and Planetary Sciences, McGill University, Montreal, Quebec, H3A 0E8, Canada 7 8 Abstract Sperrylite (PtAs2) is one of most common Pt minerals, but the processes whereby it 9 forms are not clearly established. Most commonly it is associated with the major-component 10 base metal sulfide minerals (pyrrhotite, pentlandite and chalcopyrite), which are believed to have 11 crystallized from magmatic sulfide melts. Hence, sperrylite is thought to have formed by 12 crystallization from a sulfide melt or by exsolution from sulfide minerals. However, sperrylite is 13 also found associated with silicate and oxide minerals where it is thought to have formed by 14 crystallization from the silicate magma. In order to investigate the conditions under which 15 sperrylite could crystallize from a magmatic sulfide melt we investigated sperrylite saturation in 16 Fe-Ni-Cu-S sulfide melts under controlled fO2 and fS2 at 910-1060 °C and 1 bar. The As and Pt 17 concentrations in the sulfide melt at sperrylite saturation increase from 0.23-0.41 wt% to 2.2-4.4 18 wt%, and from 0.36-0.65 wt% to 1.9-2.8 wt%, respectively, as the iron concentration in the 19 sulfide melt decreases from 50 to 36 wt% at 910-1060 ºC. We show that transitional metal 20 concentrations, particular iron and nickel, as well as sulfur and oxygen fugacities influence As 21 and Pt concentrations in the sulfide melt at sperrylite saturation.
    [Show full text]