大地测量与地球动力学
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Current Issue
2020 Vol.40 Issue.增1
Published 2020-07-22
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2017-02-14山东长岛地区出现比较集中的震群活动，后期在南侧海域又出现一系列的小震分布。本文通过双差层析成像方法重建长岛及附近海域地区的P波速度结构模型，揭示了长岛海域地震集中区及其周边区域的地壳构造特征。结果表明，南侧震群主要集中在大竹山岛-威海北断裂，与断层的走向一致；北侧震群也可能是NW向的隐伏断裂或者分支断裂。长岛南北震群附近海域的速度结构存在比较明显的速度差异，P波的速度结构横向差异比较明显，断裂带两侧介质的速度也具有明显的横向不均匀性，这也反映了高低速异常区断裂介质比较脆弱，属于应力集中释放的区域。
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