| 晚第四纪安宁河断裂的新活动与特征 |
| |
| 引用本文： | 王新民,张成贵.晚第四纪安宁河断裂的新活动与特征[J].四川地震,1997(3):8-16. |
| |
| 作者姓名： | 王新民 张成贵 |
| |
| 作者单位： | 四川省地震局 |
| |
| 摘 要： | 由２０余条次级断层组成的晚第四纪安宁河断裂是一条以左旋走滑为主兼逆冲性质的断裂。它的发育，展布，组合结构特征都与先存的南北澳断裂紧相关，并表现出明显的分段活动特性。
|
| 关 键 词： | 安宁河 断裂 活动断裂 构造分析 晚第四纪 |
NEW ACTIVITIES AND CHARACTERISTICS OF LATE QUATERNARY ANNINGHE FAULT |
| |
| Wang Xinming,Zhang Chenggui,Pei Xiyu.NEW ACTIVITIES AND CHARACTERISTICS OF LATE QUATERNARY ANNINGHE FAULT[J].Earthquake Research in Sichuan,1997(3):8-16. |
| |
| Authors: | Wang Xinming Zhang Chenggui Pei Xiyu |
| |
| Institution: | Seismological Bureau of Sichuan Province |
| |
| Abstract: | The late quaternary Anninghe fault consits of more than 20 secondary faults. It is a left-re verse-slip fault. Its characteristics about fault development, fault distribution and fault compound structure are correlate with meridional fault existed early and show a sectional activity. |
| |
| Keywords: | Anninghe fault active fault tectonic mechanical analysis |
| 本文献已被 CNKI 维普 等数据库收录！ |
