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王阅兵  金红林  付广裕 《地震》2012,32(2):121-128
2008年5月12日,青藏高原东缘龙门山断裂带发生汶川MW7.9地震,该地震使得北川—映秀断裂、灌县—江油断裂发生了同震破裂。本文主要利用震后通过复测获得的GPS同震形变场,采用Yabuki&Matsu’ura反演计算方法和分段平面断层模型,反演了地震同震滑动分布。结果表明:映秀—北川主破裂带的断层错动,在映秀附近以逆冲滑动为主,而在北川以北,其走滑运动明显大于逆冲,这一结果与震后地质调查结果与通过地震波研究获得的断层破裂特征相一致;反演得到的最大滑动量达到9.3m和9.6m,分别对应于这次地震中地表破坏最为严重的北川和映秀地区;由所获得的滑动分布计算的地震矩为8.07×1020 N.m,对应的震级为MW7.9。研究结果初步显示,Yabuki&Matsu’ura反演方法可适用在内陆地震断层反演计算中。  相似文献   
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We describe the immediate impact of the 14 November 2016 Kaikōura magnitude 7.8 (Mw) earthquake on shore platforms and cliffs around Kaikōura Peninsula. The earthquake caused an instantaneous uplift of ~1.01 m of the peninsula. We resurveyed seven profiles previously used for erosion monitoring and observed changes in the configuration of the shoreline. The coseismic uplift has fundamentally changed the process regime operating on the platforms and altered the future trajectory of shore platform and cliff development. Our observations highlight the interplay of waves, weathering, biology and tectonics. At this location tectonism strongly modulates the process regime, driving instantaneous changes in morphology and altering rates and patterns of erosion. Finally, the uplift of the Kaikōura coast has implications for changing resilience to climate change and sea level rise. Copyright © 2017 John Wiley & Sons, Ltd.  相似文献   
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??????????????????????????GPS???????????(1997-01~1999-12)??????Hori???????????????????齻????????????????????????????:????????????С??????????????????????????????7 cm/a??50%?????????????10~30 km??????????????????齻??????????????Yabuki-Matu??ura????????????????????????????Hori???????????б?????????????????????????????????????????????????в?????????Ч????????????????????????????????Hori?????????????????????????????????????????????????????????????????????????  相似文献   
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