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龙门山断裂带横断层地质特征及其控震作用

Geological Characteristics of Transverse Faults and its Earthquake-controlling Function along the Longmenshan Fault Zone

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【作者】 王伟锋卿艳彬朱传华单新建张晓杰

【Author】 WANG Wei-feng;QING Yan-bin;ZHU Chuan-hua;SHAN Xin-jian;ZHANG Xiao-jie;School of Geosciences,China University of Petroleum (Huadong);State Key Laboratory of Earthquake Dynamics,Institute of Geology,CEA;

【机构】 中国石油大学(华东)地球科学与技术学院中国地震局地质研究所地震动力学国家重点实验室

【摘要】 利用区域地质、构造、遥感地貌、地球物理、野外露头等多方面的证据,标定出龙门山断裂带横断层。在分析卧龙—怀远、虎牙断裂南段和白龙江等横断层特征及分布的基础上,探讨了横断层的控震作用。研究认为,龙门山断裂带横断层具有独立发震、使龙门山主断裂带分段活动及分段发震、与主逆冲断裂联合发震、在主震发生后控制余震传播和引发余震等多种方式的控震作用。

【Abstract】 Combining with the overall evidence of regional geology,tectonic,remote sensing landscape,geophysics and field outcrop investigating etc.,we identified the transverse faults in Longmenshan fault zone. Basing on analyzing the distribution and characteristics of transverse fault,such as Wolong-Huaiyuan Fault and southern segment of Huya Fault and Bailongjiang etc.,we discussed the earthquake-controlling function of the transverse fault. The research results showthat the transverse faults in Longmenshan Faults Zone has the earthquake- controlling function,such as causing earthquake independently,making the different segment of Longmenshan main faults active and triggering earthquakes separately,occurring earthquakes join with the main thrust faults,controlling the spread of aftershock after the main earthquake and triggering aftershocks etc..

【基金】 国家自然科学基金“基于形变场与地震波的芦山地震震源特征及发震机制研究”(41340008)资助
  • 【文献出处】 地震研究 ,Journal of Seismological Research , 编辑部邮箱 ,2015年02期
  • 【分类号】P315.2
  • 【被引频次】2
  • 【下载频次】96
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