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| 中国大陆活动断裂大震复发间隔 | |
| 引用本文： | 谢富仁,张世民,张永庆,任俊杰,张效亮,冉洪流.中国大陆活动断裂大震复发间隔[J].震灾防御技术,2013,8(1):1-10. |
| 作者姓名： | 谢富仁 张世民 张永庆 任俊杰 张效亮 冉洪流 |
| 作者单位： | 1. 中国地震局地壳应力研究所(地壳动力学重点实验室),北京,100085 2. 中国地震局地震灾害防御中心,北京,100029 3. 中国地震局地质研究所,北京,100029 |
| 基金项目： | 中国第五代地震区划图编制项目和国家科技支撑计划课题（2012BAK19B03）资助 |
| 摘 要： | 通过重新编制活动断层定量参数数据库,利用中国大陆活动断裂定量资料评估了中国大陆活动断裂(段)的大震复发间隔,给出了青藏、新疆、华北3个构造区的大震复发间隔分布特征。研究结果表明,青藏高原活动断裂M7.5级以上大震复发间隔远小于华北和新疆。青藏高原从几100a到2000a,而华北和新疆则从2000a到5000a。大震复发间隔与断层滑动速率成反比,边界断裂的大震复发间隔通常比块体内部断裂短,比例关系大体为1:1.5—2.0。大震复发间隔与断裂性质相关,走滑断层的复发间隔小于逆走滑断层,逆走滑断层小于逆断层,比例关系大体为1:1.5—2.5。现有的定量数据汇编成果和大震复发间隔估计以及统计结果,既可作为地震危险性分析的重要参数,又可作为构造类比研究的参考信息。 |
| 关 键 词： | 活动断裂 定量参数 大震 复发间隔 中国大陆 |
| 收稿时间： | 2013/2/18 0:00:00 |
Large Earthquake Recurrent Intervals along Active Faults in Mainland China |
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| Xie Furen,Zhang Shimin,Zhang Yongqing,Ren Junjie,Zhang Xiaoliang and Ran Hongliu.Large Earthquake Recurrent Intervals along Active Faults in Mainland China[J].Technology for Earthquake Disaster Prevention,2013,8(1):1-10. | |
| Authors: | Xie Furen Zhang Shimin Zhang Yongqing Ren Junjie Zhang Xiaoliang and Ran Hongliu |
| Institution: | 1) Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China;1) Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China;1) Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China;1) Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China;2) China Earthquake Disaster Prevention Center, China Earthquake Administration, Beijing 100029, China;3) Institute of Geology, China Earthquake Administration, Bijing 100029, China |
| Abstract: | By recompiling quantitative parameters database, we reassessed the large earthquake recurrent intervals along active faults in mainland China. We also obtained the large earthquake intervals distribution characteristics of active faults in Qinghai-Tibetan, Xinjiang and Northern China. The results show that the recurrent intervals of MS7.5 earthquake along active faults in Qinghai-Tibetan that is about several hundreds to 2000 years are much smaller than that of 2000 to 5000 years in Northern China and Xinjiang. The earthquake recurrent intervals are inversely proportional to the slip rate of faults. Generally, the large earthquake recurrent intervals of boundary faults are smaller than that of the faults within blocks, with a proportion about 1:1.5 to 2.0. The large earthquake recurrent intervals are also related to the type of faults, for example, strike slip faults have smaller recurrent intervals than that of reverse-strike slip faults, and reverse-strike slip faults have smaller recurrent intervals than that of reverse faults, with a proportion about 1:1.5 to 2.5. The recompiled quantitative parameter database may provide useful references not only for seismic hazard analysis, but also for the tectonic background study. |
| Keywords: | Active faults Quantitative parameters Large earthquake Recurrent intervals Mainland China |
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