An overview of chalcophile element contents of pyrrhotite, pentlandite, chalcopyrite, and pyrite from magmatic Ni-Cu-PGE sulfide deposits

Author:

Mansur Eduardo T.ORCID,Barnes Sarah-Jane,Duran Charley J.

Funder

Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Reference159 articles.

1. Alard O, Griffin WL, Lorand JP, Jackson SE, O’Reilly SY (2000) Non-chondritic distribution of the highly siderophile elements in mantle sulphides. Nature 407(6806):891–894

2. Amaral LFS (2017) The distribution of platinum-group elements and other chalcophile elements among sulfide minerals from the Ovoid ore body of the Voisey’s Bay Ni-Cu sulfide deposit, Canada. Unpubl MSc thesis, Université du Québec à Chicoutimi, 166 pp

3. Averill SA (2001) The application of heavy indicator mineralogy in mineral exploration with emphasis on base metal indicators in glaciated metamorphic and plutonic terrains. Geol Soc Lond, Spec Publ 185(1):69–81

4. Averill SA (2011) Viable indicator minerals in surficial sediments for two major base metal deposit types: Ni-Cu-PGE and porphyry Cu. Geochem: Explor Env A 11:279–291

5. Ballhaus C, Sylvester P (2000) Noble metal enrichment processes in the Merensky Reef, Bushveld Complex. J Petrol 41(4):545–561

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