| Reference Type | Journal (article/letter/editorial) |
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| Title | Serpentine minerals from two areas of the Western Australian nickel belt |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Moeskops, P. G. | Author |
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| Year | 1977 (September) | Volume | 41 |
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| Issue | 319 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_41/41-319-313.pdf+ |
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| DOI | doi:10.1180/minmag.1977.041.319.02Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 2777 | Long-form Identifier | mindat:1:5:2777:3 |
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| GUID | 0 |
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| Full Reference | Moeskops, P. G. (1977) Serpentine minerals from two areas of the Western Australian nickel belt. Mineralogical Magazine, 41 (319) 313-322 doi:10.1180/minmag.1977.041.319.02 |
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| Plain Text | Moeskops, P. G. (1977) Serpentine minerals from two areas of the Western Australian nickel belt. Mineralogical Magazine, 41 (319) 313-322 doi:10.1180/minmag.1977.041.319.02 |
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| In | (1977, September) Mineralogical Magazine Vol. 41 (319) Mineralogical Society |
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| Abstract/Notes | SummaryInvestigation of serpentine minerals from metaserpentinized ultramafic rocks in two Archaean green-stone belts, east of Kalgoorlie, has indicated that antigorite, exhibiting a very wide range of textures in thin section, is the dominant serpentine species; however, it is locally accompanied by relict lizardite. Chrysotile occurs both in late tectonic veins and as a present-day weathering product of relict olivine. Analytical data and structural formulae on seven serpentines, characterized independently by X-ray diffraction analysis, support the chemical differences between antigorite and chrysotile postulated by earlier workers. |
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