Flexural fold structures and active faults in the northern–western Weihe Graben, central China

HANDLE オープンアクセス

この論文をさがす

抄録

Field investigations and analyses of tectonic topography related to late Pleistocene–Holocene activity of faults and fault-related flexural folds in the northern–western Weihe Graben, central China, reveal that: (1) four main active faults are present in the study area, the Beishan Piedmont Fault (BPF), the Kouzhen-Guanshan Fault (KGF), the Qishan-Mazhao Fault (QMF), and the Weihe Fault (WF), of which the BPF, KGF, and WF are normal faults whereas the QMF is a left-lateral strike-slip fault; (2) active flexural folds trending ENE–WSW are widely developed on the late Pleistocene–Holocene loess tablelands and alluvial fans, as well as on terrace risers; (3) vertical slip rates on the BPF, KGF, and WF are ∼0.5–1.1 mm/yr, and the left-lateral slip rate on the QMF is ∼1.5 mm/yr; and (4) a recent seismic faulting event with a magnitude (M) > 7 occurred in the past ∼3000 yr. Our results show that active faults and fault-related flexural folds are developing in the Weihe Graben under an ongoing extensional regime, with listric faulting occurring along pre-existing faults associated with the spreading of continental crust in intracontinental graben systems around the Ordos Block.

収録刊行物

関連プロジェクト

もっと見る

詳細情報 詳細情報について

  • CRID
    1050845760751718016
  • NII論文ID
    120005704203
  • NII書誌ID
    AA11138796
  • ISSN
    13679120
  • HANDLE
    2433/204523
  • 本文言語コード
    en
  • 資料種別
    journal article
  • データソース種別
    • IRDB
    • CiNii Articles
    • KAKEN

問題の指摘

ページトップへ