Origin of hydrothermal fluids and gold mineralization associated with the Ventersdorp Contact Reef, Witwatersrand Basin, South Africa: Constraints from S, O, and H isotopes

Special Paper of the Geological Society of America

Volumn 405, Issue , 2006, Pages 333-352

  Zhao, B ^a   Robb, L J ^b   Harris, C ^c   Jordaan, L J ^d  

^a UNIVERSITY OF FORT HARE   (South Africa)

^b UNIVERSITY OF THE WITWATERSRAND   (South Africa)

^c UNIVERSITY OF CAPE TOWN   (South Africa)

^d Western Cape Regional Office   (South Africa)

Author keywords

Gold mineralization; Hydrogen isotope; Hydrothermal fluid; Oxygen isotope; Sulfur isotope; Ventersdorp contact reef; Witwatersrand

Indexed keywords

CALCITE; COPPER COMPOUNDS; GOLD DEPOSITS; ISOTOPES; MICA; PYRITES; REEFS; SULFUR COMPOUNDS; ZINC SULFIDE;

GOLD MINERALIZATION; HYDROGEN ISOTOPE; HYDROTHERMAL FLUIDS; OXYGEN ISOTOPES; SULFUR ISOTOPE; VENTERSDORP CONTACT REEFS; WITWATERSRAND;

MINERALOGY;

BASIN; CONGLOMERATE; EQUILIBRIUM; FOOTWALL; GOLD; GREENSCHIST FACIES; HYDROTHERMAL FLUID; MINERALIZATION; MUSCOVITE; OXYGEN ISOTOPE; REEF; SULFUR ISOTOPE;

SOUTH AFRICA; WITWATERSRAND;

EID: 36448963962     PISSN: 00721077     EISSN: None     Source Type: Book Series    
DOI: 10.1130/2006.2405(17)     Document Type: Article

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