2021 - 2030年中国大陆强震风险评估

Zhigang Shao , Yanqiang Wu , Lingyun Ji , Faqi Diao , Fuqiang Shi , Yujiang Li , Feng Long , Hui Zhang , Wuxing Wang , Wenxin Wei , Peng Wang , Xiaoxia Liu , Qi Liu , Zhengyang Pan , Xiaofei Yin , Yue Liu , Wei Feng , Zhenyu Zou , Jia Cheng , Renqi Lu , Xi Li
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引用次数: 7

摘要

通过对中国大陆活动构造块体边界带的研究,进行了2021~2030年地震的长期预报。基于强震复发模型,采用地震地质学、大地测量学和历史地震记录等相关研究,通过每条断层的复发期和经过时间,给出了未来10年每条目标断层的累积概率。基于世界各地大地震的长期预测,本文提出了一种基于地震间隙、运动强烈锁定、中小地震稀疏、库仑应力明显增加的断层段的综合判断方案。本文综合分析了中国大陆活动构造块体边界带主要断层未来10年可能发生强震的相对风险。每个断层的当前加载速率首先受到大地测量结果的约束;然后根据最近一次强烈地震以来经过的时间来估计每个断层的累积位移。
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Assessment of strong earthquake risk in the Chinese mainland from 2021 to 2030

The long-term earthquake prediction from 2021 to 2030 is carried out by researching the active tectonic block boundary zones in the Chinese mainland. Based on the strong earthquake recurrence model, the cumulative probability of each target fault in the next 10 years is given by the recurrence period and elapsed time of each fault, which are adopted from relevant studies such as seismological geology, geodesy, and historical earthquake records. Based on the long-term predictions of large earthquakes throughout the world, this paper proposes a comprehensive judgment scheme based on the fault segments with the seismic gap, motion strongly locked, sparse small-moderate earthquakes, and apparent Coulomb stress increase. This paper presents a comprehensive analysis of the relative risk for strong earthquakes that may occur in the coming 10 years on the major faults in the active tectonic block boundary zones in the Chinese mainland. The present loading rate of each fault is first constrained by geodetic observations; the cumulative displacement of each fault is then estimated by the elapsed time since the most recent strong earthquake.

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