地震地质 ›› 2008, Vol. 30 ›› Issue (1): 161-175.

• 专题综述 • 上一篇    下一篇

青藏高原北部活动地块内部的活断层定量资料

刘百篪1, 曹娟娟2, 袁道阳1,3, 何文贵1,3   

  1. 1. 中国地震局兰州地震研究所, 兰州, 730000;
    2. 云南省地震局, 昆明, 650224;
    3. 中国地震局兰州地震研究所, 兰州, 730000
  • 收稿日期:2007-10-24 修回日期:2008-02-19 出版日期:2008-03-19 发布日期:2009-08-24
  • 作者简介:刘百篪,男,1941年生,1964年毕业于兰州大学地质地理系地质专业,研究员,曾任国家地震局地质研究所博士生导师,中国地震学会地震地质专业委员会副主任,主要从事地震地质、活动构造、历史地震等研究,电话:0931-82767123,E-mail:liubc41@163.com.
  • 基金资助:
    国家重点基础研究发展规划项目(G199804070104)资助.中国地震局兰州地震研究所论著编号:lc20070055

QUANTITATIVE DATA OF ACTIVE FAULTS WITHIN THE ACTIVE TECTONIC BLOCK IN NORTH QINGHAI-XIZANG PLATEAU

LIU Bai-chi1, CAO Juan-juan2, YUAN Dao-yang1,3, HE Wen-gui1,3   

  1. 1. Lanzhou Institute of Seismology, CEA, Lanzhou 730000, China;
    2. Earthquake Administration of Yunnan Province, Kunming 650224, China ;
    3. Lanzhou Base of Institute of Earthquake Prediction, CEA, Lanzhou 730000, China
  • Received:2007-10-24 Revised:2008-02-19 Online:2008-03-19 Published:2009-08-24

摘要: 文中定义了祁连山活动地块的边界,列表给出了近十几年来在青藏高原北部活动地块内部的活断层定量资料。其内容主要包括:活断层的编号、名称、产状、主要的地质地貌标志、活动年代、断层分段、断层滑动速率、古地震及其年代、地震破裂带的主要特征等。这些资料表明:青藏高原北部活动地块的8级大地震集中在它的边界活断层上,断层的滑动速率都在5~12mm/a左右;7级左右的地震发生在其内部规模较小的断层上,断层的滑动速率都在1~3mm/a左右;青藏高原北部活动地块内部的活断层,可以将该活动地块划分为几个次级地块,这些次级活动地块以变形为主,没有发生旋转;我们的结果支持青藏高原"连续变形"的假说。

关键词: 青藏高原, 活动地块, 活断层, 定量资料

Abstract: This paper defines the boundaries of north Qinghai-Xizang plateau active tectonic block and offers quantitative information of active faults within the north Qinghai-Xizang plateau active tectonic block in the past dozen years. The information mainly include: the serial number,name,attitude of active fault,main geological geomorphic signs,activity age,fault segmentation,fault slip rate,paleo-earthquake and its date,and the major features of earthquake rupture zones and so on. These data indicate that great earthquakes with M≥8 concentrate on the boundary active faults of the north Qinghai-Xizang plateau active tectonic block,and the slip rate of the faults all reaches about 5~12mm/yr. Earthquakes of about M7 occurred on the smaller-scale active faults inside the north Qinghai-Xizang plateau active tectonic block. Generally,the slip rates of these active faults are 1~3mm/yr.The north Qinghai-Xizang plateau active tectonic block can be divided into several sub-blocks,and these active sub-blocks are dominated with deformation,and no rotation occurred. Our result supports the hypothesis of continuous deformation of Qinghai-Xizang plateau active tectonic block.

Key words: Qinghai-Xizang plateau, active tectonic block, active fault, quantitative data

中图分类号: