A Short Geological Review of the Bushveld Complex by R
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Mineral Profile
Platinum September 2009 Definition, mineralogy and Pt Pd Rh Ir Ru Os Au nt Atomic 195.08 106.42 102.91 192.22 101.07 190.23 196.97 deposits weight opme vel Atomic Definition and characteristics 78 46 45 77 44 76 79 de number l Platinum (Pt) is one of a group of six chemical elements ra UK collectively referred to as the platinum-group elements Density ne 21.45 12.02 12.41 22.65 12.45 22.61 19.3 (gcm-3) mi (PGE). The other PGE are palladium (Pd), iridium (Ir), osmium e Melting bl (Os), rhodium (Rh) and ruthenium (Ru). Reference is also 1769 1554 1960 2443 2310 3050 1064 na point (ºC) ai commonly made to platinum-group metals and to platinum- Electrical st group minerals, both often abbreviated to PGM. In this su resistivity r document we use PGM to refer to platinum-group minerals. 9.85 9.93 4.33 4.71 6.8 8.12 2.15 f o (micro-ohm re cm at 0º C) nt Chemically the PGE are all very similar, but their physical Hardness Ce Minerals 4-4.5 4.75 5.5 6.5 6.5 7 2.5-3 properties vary considerably (Table 1). Platinum, iridium (Mohs) and osmium are the densest known metals, being significantly denser than gold. Platinum and palladium are Table 1 Selected properties of the six platinum-group highly resistant to heat and to corrosion, and are soft and elements (PGE) compared with gold (Au). ductile. Rhodium and iridium are more difficult to work, while ruthenium and osmium are hard, brittle and almost pentlandite, or in PGE-bearing accessory minerals (PGM). -
Predictability of Pothole Characteristics and Their Spatial Distribution At
79_Chitiyo:Template Journal 12/15/08 11:16 AM Page 733 Predictability of pothole characteristics J o and their spatial distribution at u Rustenburg Platinum Mine r n by G. Chitiyo*, J. Schweitzer*, S. de Waal*, P. Lambert*, and a P. Olgilvie* l P a p Synopsis thermo-chemical erosion of the cumulus floor by new influxes of superheated magma best explains the observed data. e Prediction of pothole characteristics is a challenging task, Partial to complete melting of the cumulate floor occurred in r confronting production geologists at the platinum mines of three phases. The first represents the emplacement of hot the Bushveld Complex. The frequency, distribution, size, magma. This magma, due to turbulent flow and high chemical shape, severity and relationship (FDS3R) of potholes has a and physical potential, aggressively attacks the existing floor huge impact on mine planning and scheduling, and (crystal mush on the magma/floor interface). Regional consequently cost. It is with this in mind that this study was erosion is manifested by large, often coalescing potholes. initiated. During the second phase, when the magma emplacement Quantitative analysis of potholes indicates that pothole process ceased and cooling in situ started, two distinct size (area covered) can be described by two partly periods of pothole formation ensued. The first is related to overlapping lognormal distributions. These are referred to as rapid cooling along the relatively steep part of the Newton Populations A (smaller) and B (larger). The range of Cooling Curve, when Population B potholes nucleated observed pothole sizes conforms to a simple double randomly and grew rapidly with concurrent convective exponential growth model based on Newton’s Cooling Curve. -
Comparison of Extent and Transformation of South Africa's
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by South East Academic Libraries System (SEALS) Research in Action South African Journal of Science 97, May/June 2001 179 remote sensing applications in South Comparison of extent and Africa. This is a hierarchical framework designed to suit South African conditions, transformation of South Africa’s and incorporates known land-cover types that can be identified in a consistent woodland biome from two national and repetitive manner from high- resolution satellite imagery such as Land- databases sat TM and SPOT.The ‘natural’vegetation classes are based on broad, structural M.W. Thompsona*, E.R. Vinka, D.H.K. Fairbanksb,c, A. Ballancea types only, and are not intended to be and C.M. Shackletona,d equivalent to a floristic or ecological vege- tation classification. It is important to understand that a HE RECENT COMPLETION OF THE SOUTH Fairbanks et al.5 combination of both the NLC database’s TAfrican National Land-Cover Database This paper compares the distribution ‘Woodland’ and ‘Thicket, Bushland, and the Vegetation Map of South Africa, and location of woodland and bushveld- Bush-Clump & Tall Fynbos’ land-cover Swaziland and Lesotho, allows for the first type vegetation categories defined within classes were used in the comparison with time a comparison to be made on a national scale between the current and potential the NLC data, and the equivalent the DEAT defined ‘Savanna Biome’. The distribution of ‘natural’ vegetation resources. ‘Savanna Biome’ class defined within the inclusion of the NLC’s ‘Thicket, Bushland This article compares the distribution and DEAT’s ‘VegetationMap’ data. -
New Mineral Names*,†
American Mineralogist, Volume 104, pages 625–629, 2019 New Mineral Names*,† DMITRIY I. BELAKOVSKIY1 AND FERNANDO CÁMARA2 1Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18 korp. 2, Moscow 119071, Russia 2Dipartimento di Scienze della Terra “Ardito Desio”, Universitá di degli Studi di Milano, Via Mangiagalli, 34, 20133 Milano, Italy IN THIS ISSUE This New Mineral Names has entries for 8 new minerals, including fengchengite, ferriperbøeite-(Ce), genplesite, heyerdahlite, millsite, saranchinaite, siudaite, vymazalováite and new data on lavinskyite-1M. FENGCHENGITE* X-ray diffraction pattern [d Å (I%; hkl)] are: 7.186 (55; 110), 5.761 (44; 113), 4.187 (53; 123), 3.201 (47; 028), 2.978 (61; 135). 2.857 (100; 044), G. Shen, J. Xu, P. Yao, and G. Li (2017) Fengchengite: A new species with 2.146 (30; 336), 1.771 (36; 24.11). Single-crystal X-ray diffraction data the Na-poor but vacancy-dominante N(5) site in the eudialyte group. shows the mineral is trigonal, space group R3m, a = 14.2467 (6), c = Acta Mineralogica Sinica, 37 (1/2), 140–151. 30.033(2) Å, V = 5279.08 Å3, Z = 3. The structure was solved by direct methods and refined to R = 0.043 for all unique I > 2σ(I) reflections. Fengchengite (IMA 2007-018a), Na Ca (Fe3+,) Zr Si (Si O ) 12 3 6 3 3 25 73 Fenchengite is the Fe3+ analog of eudialyte with a structural difference (H O) (OH) , trigonal, is a new eudialyte-group mineral discovered in 2 3 2 in vacancy dominant N5 site and splitting its Na site N1 into N1a and the agpaitic nepheline syenites and its pegmatite facies near the Saima N1b sites. -
STRATIFORM and ALLUVIAL Plafl NUM MINERALIZATION in THE
LU3 The Canadian M iner alog is t Vol. 33,pp. 1023-lM5(1995) STRATIFORMAND ALLUVIALPLAfl NUM MINERALIZATION IN THENEW CALEDONIA OPHIOLITE COMPLEX THIERRY AUGE lNI PIERREMATIRZOT BRGM'Metallogeny and Geotynarnics", B.P. 6009, 45060 Orldans Cedex 2, France ABSTRA T An unusualtype offt mineralizationhas beenfound in the New Caledoniaophiolite complex, associatedwitl stratiform chromite-bearingrocks at the baseof the cumulateseries (close to the transition zone betweendunite and pyroxene-bearing rocks) and with cbromite-richpyroxenite dykes from the samezone. Two placer deposis, both enrichedin Fl also have been recognized one derived from the chromite-rich horizons and the other a cbromitiferous beach sand of unknown origin. Chromite-bearingrocks aremarked by a very strongenrichment in Pt relative to fhe other platinum-groupelements (PGE), $'ith a rrardmunconcentration of 11.5ppm (average3.9 ppm). The Pt enrichmenttakes the form of platinum-groupminerals (PGM) included in chromite crystals and is interpretedas being pdlrar'/. The following minerals have been identified: ft-Fe{u alloys (isoferroplatinum,tulame€nite, tetraferroplatinum and undeterminedphases), cooperite, laurite, bowieite, malanite, cuprorhodsite,unnamed PGE oxides, and base-metalsulfides with PGE in solid solution. The associatedplacers show a slightly different mineral association,with isoferroplatinum,tulameenite, and rare cooperite,sperrylite, Os-k-Ru alloys and PGE oxides. A more complex paragenesishas been identified in the beach san4 with isoferroplatinum,cooperite, laurite, erlichmanite, Os-Ir-Ru alloys, bowieite, ba$ite, hollingworthire, sperrylite, stibiopalladinite, and unnamed Rh sulfide, Pt-Ru-Rh alloy and PGE oxides. This type of mineralization, which differs markedly from the Os-Ru-h mineralization previously recognized in podiform cbromitite in New Caledonia, shows several analogies with Alaskan-type PGE mineralization.The host chromitite,with typical cumulustextwes, is markedby Ti and Feh emichmentdue to derivationfrom an evolved liquid. -
ECONOMIC GEOLOGY RESEARCH INSTITUTE HUGH ALLSOPP LABORATORY University of the Witwatersrand Johannesburg
ECONOMIC GEOLOGY RESEARCH INSTITUTE HUGH ALLSOPP LABORATORY University of the Witwatersrand Johannesburg CHROMITITES OF THE BUSHVELD COMPLEX- PROCESS OF FORMATION AND PGE ENRICHMENT J.A. KINNAIRD, F.J. KRUGER, P.A.M. NEX and R.G. CAWTHORN INFORMATION CIRCULAR No. 369 UNIVERSITY OF THE WITWATERSRAND JOHANNESBURG CHROMITITES OF THE BUSHVELD COMPLEX – PROCESSES OF FORMATION AND PGE ENRICHMENT by J. A. KINNAIRD, F. J. KRUGER, P.A. M. NEX AND R.G. CAWTHORN (Department of Geology, School of Geosciences, University of the Witwatersrand, Private Bag 3, P.O. WITS 2050, Johannesburg, South Africa) ECONOMIC GEOLOGY RESEARCH INSTITUTE INFORMATION CIRCULAR No. 369 December, 2002 CHROMITITES OF THE BUSHVELD COMPLEX – PROCESSES OF FORMATION AND PGE ENRICHMENT ABSTRACT The mafic layered suite of the 2.05 Ga old Bushveld Complex hosts a number of substantial PGE-bearing chromitite layers, including the UG2, within the Critical Zone, together with thin chromitite stringers of the platinum-bearing Merensky Reef. Until 1982, only the Merensky Reef was mined for platinum although it has long been known that chromitites also host platinum group minerals. Three groups of chromitites occur: a Lower Group of up to seven major layers hosted in feldspathic pyroxenite; a Middle Group with four layers hosted by feldspathic pyroxenite or norite; and an Upper Group usually of two chromitite packages, hosted in pyroxenite, norite or anorthosite. There is a systematic chemical variation from bottom to top chromitite layers, in terms of Cr : Fe ratios and the abundance and proportion of PGE’s. Although all the chromitites are enriched in PGE’s relative to the host rocks, the Upper Group 2 layer (UG2) shows the highest concentration. -
National Forests Act: List of Protected Tree Species
6 No. 37037 GOVERNMENT GAZETTE, 22 NOVEMBER 2013 GOVERNMENT NOTICES GOEWERMENTSKENNISGEWINGS DEPARTMENT OF AGRICULTURE, FORESTRY AND FISHERIES DEPARTEMENT VAN LANDBOU, BOSBOU EN VISSERYE No. 877 22 November 2013 NOTICE OFOF THETHE LISTLIST OFOF PROTECTEDPROTECTED TREE TREE SPECIES SPECIES UNDER UNDER THE THE NATIONAL NATIONAL FORESTS ACT, 19981998 (ACT(ACT NO No. 84 84 OF OF 1998) 1998) By virtue of powers vested in me under Section 15(3) of the National Forests Act, 1998, I, Tina Joemat-Pettersson, Minister of Agriculture, Forestry and Fisheries hereby publish a list of all protected trees belonging to a particular species under Section 12(1) (d) set out in Schedule below. The effect of this declaration is that in terms of Section 15(1) of the National Forests Act, 1998, no person may cut, disturb, damage or destroy any protected tree or possess, collect, remove, transport, export, purchase, sell, donate or in any other manner acquire or dispose of any protected tree or any forest product derived from a protected tree, except under a licence or exemption granted by the Minister to an applicant and subject to such period and conditions as may be stipulated. Contravention of this declaration is regarded as a first category offence that may result in a person who is found guilty of being sentenced to a fine or imprisonment for a period up to three years, or to both a fine and imprisonment. SCHEDULE A / BYLAE A Botanical Name English Other Common Names National Common Afrikaans (A), Northern SothoTree Names (NS),SouthernSotho (S),Number Tswana (T), Venda (V), Xhosa (X), Zulu (Z) Acacia erioloba Camel thorn Kameeldoring (A) / Mogohlo (NS) / 168 Mogotlho (T) Acacia haematoxylon Grey camel thorn Vaalkameeldoring (A) / Mokholo (T) 169 Adansonia digitata Baobab Kremetart (A) /Seboi (NS)/ Mowana 467 (T) Afzelia quanzensis Pod mahogany Peulmahonie (A) / Mutokota (V) / 207 lnkehli (Z) Balanites subsp. -
Comparative Wood Anatomy of Afromontane and Bushveld Species from Swaziland, Southern Africa
IAWA Bulletin n.s., Vol. 11 (4), 1990: 319-336 COMPARATIVE WOOD ANATOMY OF AFROMONTANE AND BUSHVELD SPECIES FROM SWAZILAND, SOUTHERN AFRICA by J. A. B. Prior 1 and P. E. Gasson 2 1 Department of Biology, Imperial College of Science, Technology & Medicine, London SW7 2BB, U.K. and 2Jodrell Laboratory, Royal Botanic Gardens, Kew, Richmond, Surrey, TW9 3DS, U.K. Summary The habit, specific gravity and wood anat of the archaeological research, uses all the omy of 43 Afromontane and 50 Bushveld well preserved, qualitative anatomical charac species from Swaziland are compared, using ters apparent in the charred modem samples qualitative features from SEM photographs in an anatomical comparison between the of charred samples. Woods with solitary ves two selected assemblages of trees and shrubs sels, scalariform perforation plates and fibres growing in areas of contrasting floristic com with distinctly bordered pits are more com position. Some of the woods are described in mon in the Afromontane species, whereas Kromhout (1975), others are of little com homocellular rays and prismatic crystals of mercial importance and have not previously calcium oxalate are more common in woods been investigated. Few ecological trends in from the Bushveld. wood anatomical features have previously Key words: Swaziland, Afromontane, Bush been published for southern Africa. veld, archaeological charcoal, SEM, eco The site of Sibebe Hill in northwest Swazi logical anatomy. land (26° 15' S, 31° 10' E) (Price Williams 1981), lies at an altitude of 1400 m, amidst a Introduction dramatic series of granite domes in the Afro Swaziland, one of the smallest African montane forest belt (White 1978). -
Thirty-Fourth List of New Mineral Names
MINERALOGICAL MAGAZINE, DECEMBER 1986, VOL. 50, PP. 741-61 Thirty-fourth list of new mineral names E. E. FEJER Department of Mineralogy, British Museum (Natural History), Cromwell Road, London SW7 5BD THE present list contains 181 entries. Of these 148 are Alacranite. V. I. Popova, V. A. Popov, A. Clark, valid species, most of which have been approved by the V. O. Polyakov, and S. E. Borisovskii, 1986. Zap. IMA Commission on New Minerals and Mineral Names, 115, 360. First found at Alacran, Pampa Larga, 17 are misspellings or erroneous transliterations, 9 are Chile by A. H. Clark in 1970 (rejected by IMA names published without IMA approval, 4 are variety because of insufficient data), then in 1980 at the names, 2 are spelling corrections, and one is a name applied to gem material. As in previous lists, contractions caldera of Uzon volcano, Kamchatka, USSR, as are used for the names of frequently cited journals and yellowish orange equant crystals up to 0.5 ram, other publications are abbreviated in italic. sometimes flattened on {100} with {100}, {111}, {ill}, and {110} faces, adamantine to greasy Abhurite. J. J. Matzko, H. T. Evans Jr., M. E. Mrose, lustre, poor {100} cleavage, brittle, H 1 Mono- and P. Aruscavage, 1985. C.M. 23, 233. At a clinic, P2/c, a 9.89(2), b 9.73(2), c 9.13(1) A, depth c.35 m, in an arm of the Red Sea, known as fl 101.84(5) ~ Z = 2; Dobs. 3.43(5), D~alr 3.43; Sharm Abhur, c.30 km north of Jiddah, Saudi reflectances and microhardness given. -
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. -
National Forests Act: List of Protected Tree Species
6 No.33566 GOVERNMENT GAZETTE, 23 SEPTEMBER 2010 GOVERNMENT NOTICES DEPARTMENT OF AGRICULTURE, FORSTRY AND FISHERIES No. 835 23 September 2010 NOTICE OF THE LIST OF PROTECTED TREE SPECIES UNDER THE NATIONAL FORESTS ACT, 1998 (ACT NO 84 OF 1998) By virtue of powers vested in me under Section 15(3) of the National Forests Act, 1998, I, Tina Joemat-Pe1tersson, Minister of Agriculture, Forestry and Fisheries hereby publish a list of all protected trees belonging to a particular species under Section 12(1) (d) set out in Schedule below. The effect of this declaration is that in terms of Section 15(1) of the National Forests Act, 1998, no person may cut, disturb, damage or destroy any protected tree or possess, collect, remove, transport, export, purchase, sell, donate or in any other manner acquire or dispose of any protected tree or any forest product derived from a protected tree, except under a licence or exemption granted by the Minister to an applicant and SUbject to such period and conditions as may be stipulated. Contravention of this declaration is regarded as a first category offence that may result in a person who is found guilty of being sentenced to a fine or imprisonment for a period up to three years, or to both a fine and imprisonment. SCHEDULE A I BYLAE A Botanical Name english Other Common Names National Common Afrikaans (A), Northern Sotho Tree Names (NS), Southern Sotho (S), Number Tswana (1), Venda (V), Xhosa 00. Zulu (Z) Acacia eri%ba Camel thorn . Kameeldoring (A) / Mogohlo (NS) / 168 Moa6tlh6 m· Acacia haematoxvlon Grev camel thorn Vaalkameeldoring CA) / Mokholo m 169 Adansonia digitata Baobab Kremetart (A) /Saboi (NS)/ Mowana 467 m Afzelia quanzensis Pod mahogany Peulmahonie (A) / Mutokota M / 207 Inkahli (Z) Ba/anites subsp. -
The Bushveld Igneous Complex
The Bushveld Igneous Complex THE GEOLOGY OF SOUTH AFRICA’S PLATINUM RESOURCES By C. A. Cousins, MSC. Johannesburg Consolidated Investment Company Limited A vast composite body of plutonic and volcanic rock in the central part of the Transvaal, the Bushveld igneous complex includes the platinum reef worked by Rustenburg Platinum Mines Limited and constituting the world’s greatest reserve of the platinum metals. This article describes the geological and economic aspects of this unusually interesting formation. In South Africa platinum occurs chiefly in square miles. Two of these areas lie at the the Merensky Reef, which itself forms part of eastern and western ends of the Bushveld and the Bushveld igneous complex, an irregular form wide curved belts, trending parallel to oval area of some 15,000 square miles occupy- the sedimentary rocks which they overlie, and ing a roughly central position in the province dipping inwards towards the centre of the of the Transvaal. A geological map of the Bushveld at similar angles. The western belt area, which provides the largest known has a flat sheet-like extension reaching the example of this interesting type of formation, western boundary of the Transvaal. The is shown on the facing page. third area extends northwards and cuts out- The complex rests upon a floor of sedi- side the sedimentary basin. Its exact relation- mentary rocks of the Transvaal System. This ship to the other outcrops within the basin floor is structurally in the form of an immense has not as yet been solved. oval basin, three hundred miles long and a As the eastern and western belts contain hundred miles broad.