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- W2046566361 abstract "Andesite magmatism plays a major role in continental crustal growth, but its subduction-zone origin and evolution is still a hotly debated topic. Compared with whole-rock analyses, melt inclusions (MIs) can provide important direct information on the processes of magma evolution. In this article, we synthesize data for melt inclusions hosted by phenocrysts in andesites, extracted from the GEOROC global compilation. These data show that melt inclusions entrapped by different phenocrysts have distinct compositions: olivine-hosted melt inclusions have basalt and basaltic andesite compositions, whereas melt inclusions in clinopyroxene and othopyroxene are mainly dacitic to rhyolitic. Hornblende-hosted melt inclusions have rhyolite composition. The compositions of melt inclusions entrapped by plagioclase are scattered, spanning from andesite to rhyolite. On the basis of the compositional data, we propose a mixing model for the genesis of the andesite, and a two-chamber mechanism to account for the evolution of..." @default.
- W2046566361 created "2016-06-24" @default.
- W2046566361 creator A5062700108 @default.
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- W2046566361 date "2013-02-04" @default.
- W2046566361 modified "2023-09-23" @default.
- W2046566361 title "Genesis and evolution of subduction-zone andesites: evidence from melt inclusions" @default.
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- W2046566361 doi "https://doi.org/10.1080/00206814.2013.767527" @default.
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