新潟県柏崎平野周辺における鮮新世~更新世のしゅう曲形成史

書誌事項

タイトル別名
  • Plio-Pleistocene Fold Development in the Kashiwazaki Plain and Vicinity, Niigata Prefecture.
  • ニイガタケン カシワザキ ヘイヤ シュウヘン ニ オケル センシンセイ コウシ

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抄録

From detailed stratigraphy including tephra, bio-and magneto-stratigraphy, we studied the process of folded structure development in Pliocene to early Pleistocene strata distributed in the Kashiwazaki plain and its vicinity, central Japan. Four folding phases are recognized; 1) from 2.8 to 2.4 Ma in the southern part and the southward of Chuo Hills, 2) from 2.0 to 1.5 Ma in Teradomari-Nishiyama Hills and its front area corresponding to continental shelf, 3) ca 1.0 Ma in the southern part of Chuo Hills, and 4) from 0.7 to 0.3 Ma in the northern part of Chuo and Hachikoku Hills. Besides them an active folding is observed in the eastern side of the Shinano River, the activity having commenced in latest Pleistocene.<BR>Each folding phase was relatively short lived from 0.4 to 0.5 Ma. In general, the intervals among these folding activities were geologically calm without any notable progress of folding activity. The culmination of folding activity had successively migrated eastward since last 3 Ma.

収録刊行物

  • 地学雑誌

    地学雑誌 105 (1), 88-112, 1996

    公益社団法人 東京地学協会

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