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van de Vusse, R., Powell, Roger (1983) The interpretation of pyrrhotine-pentlandite- tochilinite-magnetite-magnesite textures in serpentinites from Mount Keith, Western Australia. Mineralogical Magazine, 47 (345) 501-505 doi:10.1180/minmag.1983.047.345.11

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Reference TypeJournal (article/letter/editorial)
TitleThe interpretation of pyrrhotine-pentlandite- tochilinite-magnetite-magnesite textures in serpentinites from Mount Keith, Western Australia
JournalMineralogical MagazineISSN0026-461X
Authorsvan de Vusse, R.Author
Powell, RogerAuthor
Year1983 (December)Volume47
Issue345
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_47/47-345-501.pdf+
DOIdoi:10.1180/minmag.1983.047.345.11Search in ResearchGate
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Mindat Ref. ID3564Long-form Identifiermindat:1:5:3564:8
GUID0
Full Referencevan de Vusse, R., Powell, Roger (1983) The interpretation of pyrrhotine-pentlandite- tochilinite-magnetite-magnesite textures in serpentinites from Mount Keith, Western Australia. Mineralogical Magazine, 47 (345) 501-505 doi:10.1180/minmag.1983.047.345.11
Plain Textvan de Vusse, R., Powell, Roger (1983) The interpretation of pyrrhotine-pentlandite- tochilinite-magnetite-magnesite textures in serpentinites from Mount Keith, Western Australia. Mineralogical Magazine, 47 (345) 501-505 doi:10.1180/minmag.1983.047.345.11
In(1983, December) Mineralogical Magazine Vol. 47 (345) Mineralogical Society
Abstract/NotesAbstractThe ultramafic-hosted disseminated nickel sulphide deposit at Mount Keith, Western Australia, originally consisted of sulphide droplets and chrome spinels interstitial to olivine. During cooling, the sulphide droplets crystallized to pentlandite-pyrrhotine. Hydration and carbonation caused rimming and replacement of pentlandite-pyrrhotine by tochilinite, magnetite, and magnesite. These textures are interpreted in terms of diffusion between serpentinite matrix and the sulphide blebs.


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