Magmatic Sulfide Deposits. What are magmatic sulphide orebodies? Magmatic ore deposits are formed in association with the intrusion of mafic/ultramafic magma into (or sometimes on top of) the rocks forming the earth’s crust This magma contains more dark minerals like olivine and pyroxene than lightcoloured minerals like silicarich feldspars and quartz.
Magmatic Sulfide Deposits Geology Geochemistry And Exploration Anthony J Naldrett Anthony L Naldrett Professor Of Geology Anthony J Naldrett Google Books from Google Books
Nickelcopper sulfide deposits are the source for most of the world’s nickel and magmatic platinum group metal deposits You got to check out our lattest finds Https//wwwIslandtelluriumGems Close Vote Posted by 7 minutes ago.
Partitioning of Se, As, Sb, Te and Bi between monosulfide
The decrease of fO2 from the sulfide orebarren to orebearing magmatic systems indicates that reduction process indeed played a critical role in the genesis of.
Volcanogenic massive sulfide ore deposit Wikipedia
PDF fileChapter 1 Fundamentals of Magmatic Sulfide Deposits A J Naldrett 1 Chapter 2 The Perseverance and Mount Keith Nickel Deposits of the AgnewWiluna Belt Yilgarn Craton Western Australia Stephen J Barnes Marco L Fiorentini Paul Duuring Ben A Grguric and Caroline S Perring 51 Chapter 3 KomatiiteAssociated NiCu(PGE) Deposits.
Magmatic Sulphide Deposits Nature
11 rowsThe three most crucial factors for the formation of large and superlarge magmatic sulfide DEPOSIT TYPE ORIGIN DEPOSIT METAL RESERVMetal reserve ( Ni (Mt @ wt%) Cu (Mt @ wt%) PGE (t @ g/t) NiCu (PGE) deIntrusion relate Sudbury (Canada) 1978@12 1933@117 NiCu (PGE) de Magma conduit Noril’sk (Russia) 2320@177 12438@95 Magma conduit Pechenga (Russ 400@118 215@063.
Magmatic Sulfide Deposits Geology Geochemistry And Exploration Anthony J Naldrett Anthony L Naldrett Professor Of Geology Anthony J Naldrett Google Books
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Volcanogenic massive sulfide ore deposits also known as VMS ore deposits are a type of metal sulfide ore deposit mainly copper zinc which are associated with and created by volcanic associated hydrothermal events in submarine environments These deposits are also sometimes called volcanichosted massive sulfide (VHMS) deposits.
