| 晋获断裂带构造和地震活动特征 |
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| 引用本文： | 孙丽娜,金学申,温超,边鹏飞.晋获断裂带构造和地震活动特征[J].华北地震科学,2009,27(4):11-15. |
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| 作者姓名： | 孙丽娜 金学申 温超 边鹏飞 |
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| 作者单位： | 河北省地震局,河北,石家庄,050021 |
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| 基金项目： | 地震行业科研专项"历史地震资料补遗、可靠性及工程应用研究"，得到科技部支撑项目(编号2006Bac13b01)的赞助 |
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| 摘 要： | 晋获断裂带是华北地震区中一个次级构造单元，也是地震活动中的一个地震活动亚带。从分析该带的构造特征和地震活动特点出发，分析该带的分段性，发现变形强度由北向南递减、构造层次由北向南抬高。结合历史地震活动和现今地震活动，得出该带北段是该地震亚带主要的地震活动场所。在此基础上，由震级一时间模型对未来北段的强震活动进行预测。
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| 关 键 词： | 晋获断裂带 地震活动 构造 |
The Structure and Seismic Activity Characteristics of Jinhuo Fault Zone |
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| SUN Lina,JIN Xue-shen,WEN Chao,BIAN Peng-fei.The Structure and Seismic Activity Characteristics of Jinhuo Fault Zone[J].North China Earthquake Sciences,2009,27(4):11-15. |
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| Authors: | SUN Lina JIN Xue-shen WEN Chao BIAN Peng-fei |
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| Institution: | SUN Li-na,JIN Xue-shen,WEN Chao,BIAN Peng-fei(Earthquake Administration of Hebei Province,Shijiazhuang 050021,China) |
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| Abstract: | Jinhuo fault zone is a sub-structural unit of the earthquake zone in North China and a sub-band of seismic activity.According to analysis of structural characteristics and seismic activity characteristics,the belt partition of the Jinhuo fault zone is studied.The result shows that deformation intensity decreases from north to south,structural level improves form north to south.Historical seismic activity and present seismic activity indicate that the northern section is the main sites of seismic activity to... |
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| Keywords: | Jinhuo fault zone seismic activity structure |
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