Inversion of earthquake rupture process: Theory and applications

Yun-tai Chen, Yong Zhang, Li-sheng Xu
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Abstract

We present the theory and methods of earthquake rupture process inversion by using seismic and geodetic data, and their applications to scientific researches and earthquake emergency responses. It is shown that the knowledge obtained from these studies has much improved our understanding of the complexities of the earthquake source and causative mechanism of the earthquake disaster, and is of important reference value in earthquake disaster mitigation such as rapid earthquake emergency response. Especially since the 2008 Mw7.9 (MS8.0) Wenchuan, Sichuan, earthquake, fast and routine determination of the earthquake rupture process has been performed for significant earthquakes (MS ≥ 6.5 in China and MS ≥ 7.5 worldwide), and the results obtained are timely reported to the authorities and released to the public on the web site. The time consumed by the inversion has been reduced from more than 5 hours in 2009 to approximately 1–3 hours at present. The timely released rupture model was routinely used by the China Earthquake Administration and other authorities during the earthquake emergency responses period for destructive earthquakes, such as the 2010 Mw6.9 Yushu earthquake, the 2013 Mw6.6 Lushan earthquake, the 2014 Mw6.1 Ludian earthquake, and the 2015 Mw7.8 Gorkha, Nepal, earthquake, among the others.
地震破裂过程反演:理论与应用
介绍了利用地震和大地测量资料反演地震破裂过程的理论和方法,及其在科学研究和地震应急响应中的应用。研究结果表明,这些研究成果大大提高了我们对震源复杂性和地震灾害成因机制的认识,对地震快速应急响应等地震减灾具有重要的参考价值。特别是自2008年四川汶川Mw7.9 (MS8.0)地震以来,对重大地震(中国≥6.5,世界≥7.5)进行了地震破裂过程的快速常规测定,并及时向有关部门报告结果,并在网站上向公众发布。反演时间由2009年的5个多小时减少到目前的1-3小时左右。及时发布的断裂模型被中国地震局和其他有关部门在地震应急响应期间经常用于破坏性地震,如2010年玉树6.9级地震、2013年芦山6.6级地震、2014年鲁甸6.1级地震和2015年尼泊尔廓尔喀7.8级地震等。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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