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- W2000401295 abstract "Summary Investigation 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." @default.
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- W2000401295 date "1977-09-01" @default.
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- W2000401295 title "Serpentine minerals from two areas of the Western Australian nickel belt" @default.
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- W2000401295 doi "https://doi.org/10.1180/minmag.1977.041.319.02" @default.
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