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菲律宾棉兰老岛2019年4次MW>6.0地震断层运动模型及库仑应力传输研究
引用本文:吴少杰,杨莹辉,王泽根,熊凌艳,陈强,陈静,杨超.菲律宾棉兰老岛2019年4次MW>6.0地震断层运动模型及库仑应力传输研究[J].大地测量与地球动力学,2022,42(3):240-246.
作者姓名:吴少杰  杨莹辉  王泽根  熊凌艳  陈强  陈静  杨超
作者单位:西南石油大学地球科学与技术学院,成都市新都大道 8 号,610500,成都理工大学地质灾害防治与地质环境保护国家重点实验室,成都市二仙桥东三路 1 号,610059,西南石油大学土木工程与测绘学院,成都市新都大道 8 号,610500,西南交通大学地球科学与环境工程学院,成都市犀安路 999 号,611756
基金项目:日本宇航局数据资助项目;地质灾害防治与地质环境保护国家重点实验室开放基金;四川省科技计划
摘    要:基于雷达干涉测量技术,利用ALOS-2、Sentinel-1卫星升降轨雷达影像,获得2019-10~12发生在菲律宾棉兰老岛的4次MW>6.0地震的同震形变场,并以此形变结果为约束,反演得到4次地震的断层运动模型。综合分析发现,此次地震序列由3条断裂的破裂引起,其中2019-10-16和2019-10-31的2次地震为同一发震断裂,2019-10-31地震断层破裂区域位于2019-10-16地震断层破裂的东北延伸段,最大滑动量约为1.1 m,约为2019-10-16地震最大滑动量的2倍。2019-10-29地震由一条独立断层破裂引起,断层最大滑动量约为2.0 m。2019-12-15地震由一条东北向倾斜断层破裂引起,断层最大滑动量约为3.0 m。此外,2019-10-16地震引起2019-10-29地震显著滑动区明显的正向库仑应力传输;而2019-10-29地震显著增加了2019-10-31地震震源区域的库仑应力;前3次地震对2019-12-15地震孕震断层的库仑应力传输总和为负值,说明静态库仑应力传输可能不是此次地震触发的主要诱因。

关 键 词:棉兰老岛2019年地震序列  InSAR同震形变场  震源机制模型  库仑应力  触发关系  

Research of the Coseismic Faulting Models and Coulomb Stress Transfer of the Four MW>6.0 Earthquakes in Mindanao Island,Philippines in 2019
WU Shaojie,YANG Yinghui,WANG Zegen,XIONG Lingyan,CHEN Qiang,CHEN Jing,YANG Chao.Research of the Coseismic Faulting Models and Coulomb Stress Transfer of the Four MW>6.0 Earthquakes in Mindanao Island,Philippines in 2019[J].Journal of Geodesy and Geodynamics,2022,42(3):240-246.
Authors:WU Shaojie  YANG Yinghui  WANG Zegen  XIONG Lingyan  CHEN Qiang  CHEN Jing  YANG Chao
Affiliation:(School of Geoscience and Technology,Southwest Petroleum University,8 Xindu Road,Chengdu 610500,China;State Key Laboratory of Geohazard Prevention and Geoenvironment Protection,Chengdu University of Technology,1 Dongsan Road,Erxianqiao,Chengdu 610059,China;School of Civil Engineering and Geomatics,Southwest Petroleum University,8 Xindu Road,Chengdu 610500,China;Faculty of Geosciences and Environmental Engineering,Southwest Jiaotong University,999 Xi’an Road,Chengdu 611756,China)
Abstract:Using ALOS-2 and Sentinel-1 satellites SAR images based on the InSAR technology,we extract the coseismic surface deformation fields of the four MW>6.0 earthquakes that occurred between October to December of 2019 in Mindanao Island,Philippines.Then,we use the InSAR data to estimate the coseismic faulting model of these four earthquakes.The inversion result shows that the rupture of three individual faults are responsible for these four earthquakes.The dextral strike rupture of two adjacent segments of the same southeast dipping fault caused the two earthquakes occurred on 2019-10-16 and 2019-10-31,respectively.The maximum slip magnitude of the 2019-10-31 earthquake is about 1.1 m,which is two times of that of the 2019-10-16 earthquake.Another fault for the earthquake occurred on 2019-10-29,and the maximum slip magnitude is about 2.0 m.An additional fault characterized by predominant sinistral strike slip is the seismogenic fault of the 2019-12-15 earthquake,with a maximum slip magnitude of about 3.0 m.The calculation of the Coulomb failure stress(CFS)change indicates that the 2019-10-16 earthquake has caused significant positive CFS change in the high-slip area of the 2019-10-29 earthquake.Moreover,the 2019-10-29 earthquake also increased the CFS in the hypocenter area of the 2019-10-31 earthquake.Finally,the cumulated CFS change on the seismogenic fault of the 2019-12-15 earthquake due to the previous three earthquakes is less than zero,which suggests that the static CFS changes may be not the main triggering factor of the 2019-12-15 earthquake.
Keywords:Mindanao island earthquakes sequence in 2019  InSAR coseismic deformation field  source mechanism model  Coulomb failure stress  triggering relation
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