地震地质 ›› 1994, Vol. 16 ›› Issue (4): 429-439.

• 科研简报 • 上一篇    下一篇

岷山隆起的构造地貌学研究

赵小麟1, 邓起东1, 陈社发2   

  1. 1. 国家地震局地质研究所, 北京 100029;
    2. 中国地质大学(武汉), 武汉 430074
  • 收稿日期:1994-02-01 修回日期:1994-10-01 出版日期:1994-12-07 发布日期:2009-11-25
  • 基金资助:
    地震科学联合基金资助(91048)

TECTONIC GEOMORPHOLOGY OF THE MINSHAN UPLIFT IN WESTERN SICHUAN, SOUTHWESTERN CHINA

Zhao Xiaolin1, Deng Qidong1, Chen Shefa2   

  1. 1. Institute of Geology, SSB, Beijing 100029;
    2. China University of Geoscience (Wuhan), Wuhan 430074
  • Received:1994-02-01 Revised:1994-10-01 Online:1994-12-07 Published:2009-11-25

摘要: 岷山隆起为一第四纪强烈抬升区,构成川西高原的西界。岷山隆起的东、西边界分别受岷江断裂与虎牙断裂的控制,为地震活动带,南部向龙门山构造带过渡。岷江断裂北段的第四纪活动始于距今2Ma以前,为一逆走滑断层,观测到的左旋位移量为2.4km,左旋滑动速率为1mm/a.岷江断裂控制了沿隆起西界分布的地震活动,包括1933年叠溪和1960年漳腊地震。

关键词: 四川, 岷山隆起, 岷江断裂, 虎牙断裂, 构造地貌

Abstract: The NS-trending Minshan mountain in Northwestern Sichuan is an active Quatemay uplift.Its western and eastern boundaries are controlled by the active Minshan and Huya faults, respectively. The northern segment of Minshan fault has been active since 2 Ma ago. It is a reverse fault with left-lateral strike-slip component. The strike-slip displacement is about 2.4 km with a 1mm/a slip rate since 2 Ma, determined by matching offset placer gold mine with its mother lode. The Minshan and Huya faults are the major seismogenic structures in the region.

Key words: Sichuan, Minshan uplift, Minjiang fault, Huya fault, Tectonic geomor phology