Coeval volcanism due to interaction of back-arc basin basalt (BABB) magma with the island-arc crust in the late Miocene Engaru volcanic field, northeastern Hokkaido, Japan : The evidence of Sr and Nd isotopic ratios combined with major- and trace-element compositions

ZC_105(9)_625-642

WEKO3

lat lon distance

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ZC_105(9)_625-642.pdf

https://niigata-u.repo.nii.ac.jp/record/3223/files/ZC_105(9)_625-642.pdf

ZC_105(9)_625-642.pdf

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