<SPAN lang=EN-US style="FONT-SIZE: 14pt; COLOR: black; FONT-FAMILY: ’Times New Roman’; mso-fareast-font-family: 宋体; mso-font-kerning: 1.0pt; mso-ansi-language: EN-US; mso-fareast-language: ZH-CN; mso-bidi-language: AR-SA">Active Fault Movement and Recent Tectonic Stress Field in <?xml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">Yanhuai</st1:PlaceName> <st1:PlaceType w:st="on">Basin</st1:PlaceType></st1:place></SPAN>

Active Fault Movement and Recent Tectonic Stress Field in oft-com:office:smarttags" />Yanhuai Basin

详细信息

责任者：Xie Furen (Institute of Crustal Dynamics ; China Earthquake Administration ; Beijing 100085 ; China) ; Zhang Hongyan
刊名：Seismology and Geology
出版年：2007
卷期：29(4)
关键词：活动断层 ; active faults ; 构造应力场 ; tectonic stress field ; 山西 ; Shanxi Province
页码：p.693-705
图表：6 illus., 2 tables, 21 refs.
分类号：0300
issnNo：ISSN0253-4967
isbnNo：CN11-2192/P

摘要

Yanhuai oft-com:office:smarttags" />Basin contains Yanfan Basin and Huaizhuo Basin, which are connected one another. According to field seismo-geological investigation and fault slip observation, the active faults in northeast direction in Yanfan Basin are mainly dextral strike-slip, with some cases of normal fault. But in Huaizhuo Basin, the situation is opposite; the active faults in northeast direction are mainly normal faults, with some cases of strike slip. However, in the whole Yanhuai Basin, the active faults in northwest direction are mostly sinistral strike-slip, also with some cases of normal fault. By field investigation and observation, the authors got 337 data of active fault slickenside. And using the method of inversion of fault slip data, the authors can obtain the following characteristics of recent tectonic stress field in the research region.

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