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• W2003847482 abstract "Green clinopyroxenes, commonly rounded and anhedral and richer in Fe, Na and Mn than the pyroxenes of the surrounding groundmass are a common feature of mafic alkaline volcanic rocks (e.g. basanites, monchiquites, leucitites). Some are accompanied by one or more of the following phases: Fe-rich kaersutite and biotite, anorthoclase, sodic plagioclase, apatite, magnetite, sphene, which are believed to be cognate with the green pyroxenes. We review evidence that these minerals have crystallized from mugearite, trachyte or phonolite magmas, and their presence in mafic alkaline rocks is due to magma mixing. The intermediate and salic magmas may sometimes be generated at mantle depths, possibly by melting of mantle material enriched in Fe, Na and volatiles." @default.
• W2003847482 created "2016-06-24" @default.
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• W2003847482 date "1978-12-01" @default.
• W2003847482 modified "2023-09-24" @default.
• W2003847482 title "Magma mixing in mafic alkaline volcanic rocks: the evidence from relict phenocryst phases and other inclusions" @default.
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• W2003847482 doi "https://doi.org/10.1016/0377-0273(78)90020-3" @default.
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