[in Japanese]
2013 Volume 72 Issue 1 Pages 2
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The Miocene Ushikiri Formation, a 14 Ma submarine slope deposit, contains sediment gravity flow and slide deposits. Some submarine slides may have been triggered by turbidity currents.
Renkon
Taisekigaku Kenkyu
Newsletter of Japanese Association of Sedimentologists
Journal of the Sedimentological Society of Japan
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