联合测震和GPS资料反演双溪-焦溪垟断裂运动特征Inversion of movement characteristics of Shuangxi-jiaoxilang fault joint using seismic and GPS data
龚俊,汪贞杰,戴煜暄
摘要(Abstract):
针对GPS应用于监测双溪-焦溪垟断裂的运动特征的问题,通过分析文成县和泰顺县交界地区8个测震台和长达12 a 2个跨断层的GPS观测资料,分别采用CAP方法与大地线和沿该断裂进行投影得到的时间序列进行分析,得到测震和GPS一致的观测结果。研究表明:2014年震群期间,双溪-焦溪垟断裂具有右旋走滑特征,位错约4 mm; GPS观测具有长期稳定的优势,对揭示地球物理过程具有重要意义;GPS观测的误差为毫米级,对于运动量很小的断裂通过长期观测和不同方向的分解等方法可以监测到细微变形特征;对于具有震群性质的小地震(震级大于或等于3级、小于5级),GPS依然可以提供断裂地表破裂的绝对值。
关键词(KeyWords): 双溪-焦溪垟断裂;CAP;震源机制;震群;GPS;地表破裂
基金项目(Foundation): 浙江省地震局科技项目(2020ZJJ04);浙江省地震局“水库地震研究”科技创新团队资助项目
作者(Author): 龚俊,汪贞杰,戴煜暄
DOI: 10.16251/j.cnki.1009-2307.2021.12.001
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