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- W2361708558 abstract "This paper summarized the geological and geochemical features of the Muruntau gold deposit,the largest orogenic-type gold deposit in the world with gold reservoir of 6100 t.The ore bodies locate at the intersection of shear zones and faults.The wall-rock of the gold veins is black carbon schist of Upper Ordovician-lower Silurian.Alaskite(~287 Ma),occurring beneath the Muruntau ore body,had been extensively altered.Igneous dikes(273-286 Ma)expose in the north of the ore region.Native gold grains occur in quartz veins.Geochemistry of the alteration assemblages and the ores suggested magmatic contributions of the ore-forming fluid in some degree.The fluid inclusion analysis,however,implied that overwhelming majority of He came from continental crust,and the noble gases were from atmosphere.Age of gold mineralization had been determined to be ~275 Ma(Sm-Nd isochrone),226-254 Ma(sericite 40Ar/39Ar plateau)and ~290 Ma(arsenopyrite Re-Os).It requires special mechanisms and prolonged fluid evolution for such a giant ore deposit to form within a short time span and within a limited area.Shear zones,which control the terminal location of the Muruntau gold deposit,are the widespread signals and exploration indicators for gold deposits in the Central Asian Metallogenic area." @default.
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- W2361708558 date "2008-01-01" @default.
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- W2361708558 title "Geology and Geochemistry of Muruntau Gold Deposit" @default.
- W2361708558 hasPublicationYear "2008" @default.
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