Platinum-group elements in the UG1 and UG2 chromitites, and the Bastard reef, at Impala platinum mine, western Bushveld Complex, South Africa: Evidence for late magmatic cumulate instability and reef constitution

South African Journal of Geology

Volumn 111, Issue 2-3, 2008, Pages 159-176

  Maier, Wolf D ^a   Barnes, Sarah Jane ^b  

^a UNIVERSITY OF WESTERN AUSTRALIA   (Australia)

^b UNIVERSITÉ DU QUÉBEC À CHICOUTIMI   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

CHROMITITE; CORRELATION; CUMULATE; DIKE; FOOTWALL; HANGING WALL; HYDROTHERMAL FLUID; MAGMA CHAMBER; MAGMATIC DIFFERENTIATION; PLATINUM GROUP ELEMENT; SOLIDIFICATION;

AFRICA; BASTARD REEF; BUSHVELD COMPLEX; MERENSKY REEF; SOUTH AFRICA; SOUTHERN AFRICA; SUB-SAHARAN AFRICA;

AEPYCEROS MELAMPUS;

EID: 59349085357     PISSN: 10120750     EISSN: None     Source Type: Journal    
DOI: 10.2113/gssajg.111.2-3.159     Document Type: Article

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