2013年芦山地震导致的周边断层应力变化及其与2008年汶川地震的关系
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摘要
2013年4月20日,四川雅安-芦山地区发生了Ms7.0级强震,地震造成了重大的人员伤亡和经济损失.判断余震可能发生的区域、圈定震区周边未来可能发生地震活动的范围,对灾区人员安置、灾后恢复重建,以及加强震灾及次生灾害防御具有重要的参考价值.本文利用弹性位错理论和分层岩石圈模型,计算汶川地震和芦山地震引起的同震及震后粘弹松弛应力场变化,讨论了Mw7.9级汶川地震与芦山地震之间的关系、芦山地震对余震分布的影响以及汶川地震和芦山地震对周边主要活动断层的影响.结果表明:(1)汶川地震在芦山地震震中导致的库伦应力增量为0.0037~0.0114MPa,最高可能达到0.0114MPa,汶川地震可能有效地促进了芦山地震的发生.(2)芦山地震所导致的同震库伦应力场变化能够较好地解释目前余震的分布.在芦山地震破裂面东北和西南两端的应力增强区域内还没有余震记录,这些区域未来发生余震的危险性较大,需密切关注.(3)鲜水河断裂康定-道孚段、北川-映秀断裂、彭县-灌县断裂以及雅安断裂上的库伦应力增量进一步提升,地震危险性有所增强.
引文
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