鉱脈の方向から推定された広域応力場

書誌事項

タイトル別名
  • Neogene regional stress field inferred from the pattern of ore veins in Hokkaido, Japan
  • 北海道における中期中新世以降の鉱脈の例
公開日
1986
DOI
  • 10.11456/shigenchishitsu1951.36.209
公開者
資源地質学会

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説明

Neogene stress field in Hokkaido has been analyzed, based on the strikes of ore veins. The ore veins formed during the period from late Middle Miocene to Recent are taken into account. Those of E-W and ENE-WSW directions are predominant in both northeast and southwest Hokkaido.<BR>The major veins of thirteen representative mines are formed in the conjugate shear fractures, that is, E-W or ENE-WSW dextral and NW-SE sinistral. The estimated stress field is NW-SE or WNW-ESE compressional and parallel to the direction of the subducting Pacific Plate, even at ore-forming period. The predominance of E-W and ENE-WSW dextral shears might be related to the oblique subduction of the Pacific Plate.

収録刊行物

  • 鉱山地質

    鉱山地質 36 (197), 209-218, 1986

    資源地質学会

被引用文献 (2)*注記

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詳細情報 詳細情報について

  • CRID
    1390282681505043584
  • NII論文ID
    130003639697
  • DOI
    10.11456/shigenchishitsu1951.36.209
  • ISSN
    00265209
  • データソース種別
    • JaLC
    • CiNii Articles
    • Crossref
  • 抄録ライセンスフラグ
    使用不可

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