12 May 2008 M=7.9 Wenchuan, China, earthquake calculated to increase failure stress and seismicity rate on three major fault systems

被引:260
|
作者
Toda, Shinji [1 ]
Lin, Jian [2 ]
Meghraoui, Mustapha [3 ]
Stein, Ross S. [4 ]
机构
[1] AIST, Geol Survey Japan, Act Fault Res Ctr, Tsukuba, Ibaraki 3058567, Japan
[2] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA
[3] EOST, Inst Phys Globe, F-67084 Strasbourg, France
[4] US Geol Survey, Menlo Pk, CA 94025 USA
关键词
D O I
10.1029/2008GL034903
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Wenchuan earthquake on the Longmen Shan fault zone devastated cities of Sichuan, claiming at least 69,000 lives. We calculate that the earthquake also brought the Xianshuihe, Kunlun and Min Jiang faults 150-400 km from the mainshock rupture in the eastern Tibetan Plateau 0.2-0.5 bars closer to Coulomb failure. Because some portions of these stressed faults have not ruptured in more than a century, the earthquake could trigger or hasten additional M > 7 earthquakes, potentially subjecting regions from Kangding to Daofu and Maqin to Rangtag to strong shaking. We use the calculated stress changes and the observed background seismicity to forecast the rate and distribution of damaging shocks. The earthquake probability in the region is estimated to be 57-71% for M >= 6 shocks during the next decade, and 8-12% for M >= 7 shocks. These are up to twice the probabilities for the decade before the Wenchuan earthquake struck.
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页数:6
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