Finding of metamorphic rock fragments in rhyolitic tuff beds of the Oligocene Momijiyama Formation, central Hokkaido, Japan: implications in the Paleogene tectonism of central Hokkaido. | Zendy

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Finding of metamorphic rock fragments in rhyolitic tuff beds of the Oligocene Momijiyama Formation, central Hokkaido, Japan: implications in the Paleogene tectonism of central Hokkaido.

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