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- W1998099430 abstract "Summary The clino-ferrosilite from the lithophysae in an obsidian from Lake Naivasha, Kenya, originally examined by Bowen (1935), has been shown to be substantially pure FeSiO 3 , with about 5% MnSiO 3 in solid solution. It has the same space-group, P2 1 /c, as clino-enstatite and pigeonite. The unit-cell dimensions are a = 9.718 Å, b = 9·088 Å, c = 5·239 Å, β = 108° 27′. These do not conform to the scheme proposed by Brown (1960): reasons are given why this was not unexpected." @default.
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- W1998099430 date "1965-01-01" @default.
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- W1998099430 title "Re-investigation of clino-ferrosilite from Lake Naivasha, Kenya" @default.
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- W1998099430 doi "https://doi.org/10.1180/minmag.1965.034.268.05" @default.
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