High-Mg andesite produced by mixing of primitive basalt and dacite magmas, from Mikasayama, northern Hokkaido, Japan.
Keiji Wãda, Yoshihiko Goto
Abstract
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Keiji Wãda, Yoshihiko Goto
Abstract
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We found high-Mg andesite (56.5 wt.% SiO2 and 7.2 wt.% MgO) from Mikasayama in Wassamu town, northern Hokkaido.Its K-Ar age is 11.1•}0.8Ma.The high-Mg andesite is characterized by co-existence of Fo-rich olivine (Fo90-85) and An-poor plagioclase (An64-38) phenocrysts.The mineralogical evidence suggests that the high-Mg andesite from Mikasayama was produced by mixing of primitive basalt magma, containing Mg-rich olivine and clinopyroxene phenocrysts, and hornblende dacite magma.
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We found high-Mg andesite (56.5 wt.% SiO2 and 7.2 wt.% MgO) from Mikasayama in Wassamu town, northern Hokkaido.Its K-Ar age is 11.1•}0.8Ma.The high-Mg andesite is characterized by co-existence of Fo-rich olivine (Fo90-85) and An-poor plagioclase (An64-38) phenocrysts.The mineralogical evidence suggests that the high-Mg andesite from Mikasayama was produced by mixing of primitive basalt magma, containing Mg-rich olivine and clinopyroxene phenocrysts, and hornblende dacite magma.
Key concepts: Phenocryst, Andesite, Dacite, Basaltic andesite, Basalt, Geology, Geochemistry, Igneous differentiation