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Signature of Fault Healing in an Aftershock Sequence? The 2008 Wenchuan Earthquake

机译:余震序列中的故障修复签名? 2008年汶川地震

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We analyzed the aftershock sequence of the 2008 Wenchuan earthquake from May 12, 2008 to May 12, 2013 using the earthquake catalog of the China Earthquake Networks Center (CENC). In the analysis performed, we took under consideration the temporary variation in the completeness of the earthquake catalog just after the Wenchuan mainshock. The cutoff completeness magnitude from May 12 to June 27, 2008 was above 3.0 due to the impact of the earthquake sequence on the seismological observatory practice. It was observed that the b value has an increasing trend from June 27, 2008 to late April 2009, while since May 2009, the b value has remained stable. If these characteristics were associated with the possible signature of fault healing, the 'apparent healing time' could be pinpointed by this measure as around 1 year. Due to two strong asperities present on the rupture of the Wenchuan mainshock, the aftershock zone can be divided into two segments, namely the north and the south segment. The b values of the two segments seem to show different trends of temporal variation. The main contribution of the increasing trend comes from the south segment, or the 'initiation segment' of the main rupture.
机译:我们使用中国地震网络中心(CENC)的地震目录分析了2008年5月12日至2013年5月12日的2008年汶川地震的余震序列。在进行的分析中,我们考虑了汶川特大地震发生后地震目录完整性的暂时变化。由于地震序列对地震观测台做法的影响,2008年5月12日至6月27日的截止完整性等级大于3.0。从2008年6月27日至2009年4月下旬,b值呈上升趋势,而自2009年5月以来,b值保持稳定。如果这些特征与断层愈合的可能特征相关联,则该措施可以将“表观愈合时间”确定为大约一年。由于汶川主震破裂时存在两个强烈的隆起,因此余震带可分为两个部分,即北段和南段。两个片段的b值似乎显示出不同的时间变化趋势。上升趋势的主要贡献来自南段,或主要破裂的“初始段”。

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