李皓, 潘晖, 温超, 冉志杰, 吕国军. 磁县断裂带的构造和地震活动特征[J]. 华北地震科学, 2013, 31(2): 29-34. DOI: 10.3969/j.issn.1003-1375.2013.02.006
引用本文: 李皓, 潘晖, 温超, 冉志杰, 吕国军. 磁县断裂带的构造和地震活动特征[J]. 华北地震科学, 2013, 31(2): 29-34. DOI: 10.3969/j.issn.1003-1375.2013.02.006
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LI Hao, PAN Hui, WEN Chao, RAN Zhi-jie, LV Guo-jun. CHARACTERISTICS OF TECTONIC ACTIVITY AND SEISMICITY OF CIXIAN FAULT[J]. North China Earthquake Sciences, 2013, 31(2): 29-34. DOI: 10.3969/j.issn.1003-1375.2013.02.006
Citation: LI Hao, PAN Hui, WEN Chao, RAN Zhi-jie, LV Guo-jun. CHARACTERISTICS OF TECTONIC ACTIVITY AND SEISMICITY OF CIXIAN FAULT[J]. North China Earthquake Sciences, 2013, 31(2): 29-34. DOI: 10.3969/j.issn.1003-1375.2013.02.006
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磁县断裂带的构造和地震活动特征

CHARACTERISTICS OF TECTONIC ACTIVITY AND SEISMICITY OF CIXIAN FAULT

    摘要
  • 摘要: 磁县断裂带是华北地震区中重要的断裂之一,1830年该断裂带发生了M7级地震。从分析该带的构造特征和地震活动特征出发,在结合历史地震活动和现今地震活动基础上,利用震级-时间模型对磁县断裂带未来强震活动进行预测,结果表明,未来该段中南的总体活动水平维持在5级左右。

     

    Abstract: The Cixian fault zone is one of the important earthquake faults in North China, a M7 earthquake occurred in the fault in 1830.Based on the tectonic characteristics and historical and present seismic activity, we use the magnitude-time model to calculate the probability of seismicity of Cixian fault in the future.

     

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