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- W4283519143 endingPage "105312" @default.
- W4283519143 startingPage "105312" @default.
- W4283519143 abstract "The Hida Gaien Belt in southwest Japan consists mainly of Paleozoic to Mesozoic shelf-facies rocks and records the tectonic evolution of East Asia. Here we report a study of the geochemistry of mafic volcanic rocks from the Early Carboniferous Arakigawa Formation of this belt. Two types of mafic volcanic rock are identified: (1) high-Al basaltic lavas, which were generated by island arc tholeiitic magma that formed under high-pressure conditions near the crust–mantle boundary and in which the nucleation of plagioclase was suppressed and delayed; and (2) basaltic andesitic lavas, which were generated by fractional crystallization of the high-Al tholeiitic magma. Combining our new results with previous geological findings, we consider that the tectonic setting of proto-Japan during the Early Carboniferous was a primitive island arc characterized by active island arc tholeiitic magmatism and the absence of a granitic batholith." @default.
- W4283519143 created "2022-06-27" @default.
- W4283519143 creator A5017460866 @default.
- W4283519143 creator A5023122619 @default.
- W4283519143 creator A5078111213 @default.
- W4283519143 creator A5080375062 @default.
- W4283519143 date "2022-09-01" @default.
- W4283519143 modified "2023-10-17" @default.
- W4283519143 title "Magmatism and tectonic setting of proto-Japan during the Early Carboniferous: Constraints from the geochemical characteristics of mafic volcanic rocks in the Hida Gaien Belt, SW Japan" @default.
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