Depositional age of the Tertiary Kuma Group, Shikoku, and its significance

Cenozoic clastic sediments in the Kuma area, Shikoku, southwest Japan, previously designated as the Kuma Group, are here redefined as the Hiwada-toge Formation and the overlying Kuma Group sensu stricto, considering a significant time-gap between them. The Hiwada-toge Formation is Early Eocene in ag...

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Veröffentlicht in:Chishitsugaku zasshi 1999/04/15, Vol.105(4), pp.305-308
Hauptverfasser: Narita, Koichiro, Yamaji, Atsushi, Tagami, Takahiro, Kurita, Hiroshi, Obuse, Akiko, Matsuoka, Kazumi
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Sprache:eng ; jpn
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