島根県隠岐郡布施周辺の古第三紀時張山累層 The Paleogene Tokibad Fomation around Fuse, Oki Islands

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著者

    • 山内 靖喜 Yamauchi Seiki
    • 島根大学総合理工学部地球資源環境学科 Shimane University, Interdisciplinary Faculty of Science and Engineering, Department of Geoscience
    • 中山 勝博 Nakayama Katsuhiro
    • 島根大学総合理工学部地球資源環境学科 Shimane University, Interdisciplinary Faculty of Science and Engineering, Department of Geoscience

抄録

The Paleogene Tokibariyama Formation around Fuse,Oki Dogo Island is divided into 7 members.The lowest member is a talus basal conglomerate which shows the facies of sediments at a foot of a steep cliff,and lower members abut agaist steep wall of their basement rocks.These facts show that the sedimentary basin have resulted from depression caused by faulting.Volcanic clasts in debris flow deposits at the upper part of the talus basal conglomerate implies that near the study area any other volcano-pulutonic activity had taken placed prior to sedimentation of the talus basal conglomerate.Probably several volcano-pulutonic activities occured during the Tokibariyama Formation stage.

収録刊行物

  • 島根大学地球資源環境学研究報告

    島根大学地球資源環境学研究報告 14, 81-88, 1995-12-25

    島根大学総合理工学部地球資源環境学教室

各種コード

  • NII論文ID(NAID)
    110006940144
  • NII書誌ID(NCID)
    AA11455176
  • 本文言語コード
    JPN
  • 資料種別
    Departmental Bulletin Paper
  • ISSN
    13439774
  • データ提供元
    NII-ELS  IR 
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