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基于非均匀地壳模型的格林函数法反演2001年昆仑山口西Ms8.1地震的同震滑移
引用本文:周宇,聂兆生,贾治革,陈正松,杨少敏.基于非均匀地壳模型的格林函数法反演2001年昆仑山口西Ms8.1地震的同震滑移[J].大地测量与地球动力学,2012,32(3):22-26.
作者姓名:周宇  聂兆生  贾治革  陈正松  杨少敏
作者单位:中国地震局地震研究所(地震大地测量实验室),武汉,430071
基金项目:中国地震局地震行业科研专项
摘    要:建立基于地壳不均匀的三维有限元模型,将昆仑山口西Ms8.1地震产生的长约400 km的破裂带在走向上分为16段,生成各个破裂段滑移相对于地表位移的格林函数,并以GPS观测的水平位移为约束,用阻尼最小二乘法反演破裂滑移分布,结果表明反演结果与地质考察的地表破裂数据接近.用反演结果重构的地表位移场与观测值一致,并体现了断裂...

关 键 词:有限元  最小二乘法  昆仑山口西Ms8.1地震  同震滑移  GPS

INVERSION OF COSEISMIC SLIP DISTRIBUTION OF 2001 Ms8.1 KUNLUN EARTHQUAKE FROM GPS OBSERVATIONS WITH GREEN'S FUNCTION METHOD BASED ON A HETEROGENEOUS CRUST MODEL
Zhou Yu , Nie Zhaosheng , Jia Zhige , Chen Zhengsong , Yang Shaomin.INVERSION OF COSEISMIC SLIP DISTRIBUTION OF 2001 Ms8.1 KUNLUN EARTHQUAKE FROM GPS OBSERVATIONS WITH GREEN'S FUNCTION METHOD BASED ON A HETEROGENEOUS CRUST MODEL[J].Journal of Geodesy and Geodynamics,2012,32(3):22-26.
Authors:Zhou Yu  Nie Zhaosheng  Jia Zhige  Chen Zhengsong  Yang Shaomin
Institution:(Key Laboratory of Earthquake Geodesy,Institute of Seismology,CEA,Wuhan 430071)
Abstract:2001 Kunlun Ms8.1 earthquake ruptured as long as about 400 km.The displacement gradient perpendicular to the strike of rupture belt is significantly greater on the south side than that on the north.This fact cannot be explained by Okada model which is based on elastically homogeneous half space.A horizontally and vertically heterogeneous 3D-FEM model is established to generate Green’s functions of slip on 16 segments of the rupture belt with respect to the ground displacement field.With the damping LS(least square) algorithm,the slip distribution of rupture is inversed from observed horizontal displacements of 40 GPS sites,and the result is in good agreement with that from geological field investigation.The ground displacement field rebuilt by the inversed result is close to that observed by GPS,demonstrating different deformation patterns on the two sides of the rupture.
Keywords:finite element  least square algorithm  Kunlun Ms8  1 earthquake  coseismic slip  GPS
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