O- and H-isotope study of the Carbon Leader Reef at the Tau Tona and Savuka mines (Western Deep Levels), South Africa: Implications for the origin and evolution of Witwatersrand Basin fluids

South African Journal of Geology

Volumn 113, Issue 1, 2010, Pages 73-86

  Grove D ^a,b   Harris, C ^a  

^a UNIVERSITY OF CAPE TOWN   (South Africa)

^b AngloGold Ashanti Limited   (South Africa)

Author keywords

[No Author keywords available]

Indexed keywords

BASIN EVOLUTION; CONGLOMERATE; GOLD; GREENSCHIST FACIES; HYDROGEN ISOTOPE; HYDROTHERMAL FLUID; ISOTOPIC COMPOSITION; METAMORPHISM; MINERALIZATION; ORE DEPOSIT; OXYGEN ISOTOPE; QUARTZITE;

SOUTH AFRICA; WITWATERSRAND;

EID: 77956052101     PISSN: 10120750     EISSN: None     Source Type: Journal    
DOI: 10.2113/gssajg.113.1-73     Document Type: Article

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