Comparing orthomagmatic and hydrothermal mineralization models for komatiite-hosted nickel deposits in Zimbabwe using multiple-sulfur, iron, and nickel isotope data

Mineralium Deposita

Volumn 49, Issue 1, 2014, Pages 75-100

  Hofmann, Axel ^a   Bekker, Andrey ^b,c   Dirks, Paul ^d   Gueguen, Bleuenn ^e,f   Rumble, Doug ^c   Rouxel, Olivier J ^f  

^a UNIVERSITY OF JOHANNESBURG   (South Africa)

^b UNIVERSITY OF MANITOBA   (Canada)

^c GEOPHYSICAL LABORATORY   (United States)

^d JAMES COOK UNIVERSITY   (Australia)

^e UNIVERSITÉ DE BRETAGNE OCCIDENTALE   (France)

^f IFREMER   (France)

Author keywords

Archean; Iron isotopes; Komatiite hosted nickel deposit; Nickel isotopes; Sulfur isotopes; Zimbabwe craton

Indexed keywords

ARCHEAN; HIGH TEMPERATURE; HYDROTHERMAL DEPOSIT; HYDROTHERMAL FLUID; IRON ORE; ISOTOPIC FRACTIONATION; KOMATIITE; MINE; MINERALIZATION; NICKEL; ORE DEPOSIT; SULFUR ISOTOPE;

ZIMBABWE CRATON;

EID: 84892485721     PISSN: 00264598     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00126-013-0476-1     Document Type: Article

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