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- W2083323311 abstract "Several occurrences of quartzo‐feldspathic gneiss forming part of the Palaeoproterozoic Willyama Supergroup in the Olary Domain, South Australia, retain textural indications for a felsic volcanic origin. These examples preserve relict quartz phenocrysts ('quartz eyes') and, at a few sites, relict feldspar phenocrysts and fragmental textures are retained. The rocks contain an assemblage of albite and quartz, with minor muscovite, biotite, K‐feldspar, magnetite, hematite, pyrite, zircon and xenotime. They share chemical characteristics with other felsic gneisses in the Willyama Supergroup with U‐Pb zircon ages of ca 1700 Ma which have been inferred to have formed from A‐type rhyolite precursors. It is interpreted that the rocks represent rhyolitic pyroclastic or epiclastic deposits (with associated minor iron‐formation and cherty exhalites), which subsequently underwent pre‐ and/or syn‐metamorphic Na (‐Fe) metasomatism and amphibolite‐grade metamorphism." @default.
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- W2083323311 date "1998-12-01" @default.
- W2083323311 modified "2023-09-26" @default.
- W2083323311 title "Volcanic textures in quartzo‐feldspathic gneiss of the Willyama Supergroup, Olary Domain, South Australia" @default.
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- W2083323311 doi "https://doi.org/10.1080/08120099808728451" @default.
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