Exit of the water of the Nara Basin in early Pleistocene, deduced from stratigraphy and paleocurrent directions of the Osaka Group in the Sekiya area, Nara Prefecture, Japan | Zendy

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Exit of the water of the Nara Basin in early Pleistocene, deduced from stratigraphy and paleocurrent directions of the Osaka Group in the Sekiya area, Nara Prefecture, Japan

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