Joint Inversion of GPS and Gravity Data for Crustal
Movement in Fujian Area
1 Xiamen Research Centre of Seismologic Surveying, 669 Shengguang Road, Xiamen 361021, China
2 Xiamen Seismostation,Earthquake Administration of Fujian Province,9 Shiquan Road, Xiamen 361003, China
Abstract High precision GPS horizontal velocities of GPS seismic monitoring network and gravity data were used to estimate the block motion and major fault slip rate in Fujian Area.The results are as follows: Due to the influence of collision of the Eurasian, Philippine Sea and Pacific plates, crustal deformation of blocks in Fujian area are prominently in a clockwise rotation.Further, this leads to left-slip motion along the NE-striking faults and right-slip motion along the NW-striking faults. The Changle-Zhaoan, Shaowu-Heyuan and Yongan-Jinjiang faults are the most active left-lateral faults in the region, with a rate of 0.7±1.3mm/a, 0.7±1.7mm/a and 0.6±1.8 mm/a respectively, and the Jiulong river downstream area has a right-lateral slip rate of 0.5±1.7mm/a.
ZHAN Hui,LIANG Quanqiang,ZHOU Hongwei et al. Joint Inversion of GPS and Gravity Data for Crustal
Movement in Fujian Area[J]. jgg, 2015, 35(1): 16-20.
ZHAN Hui,LIANG Quanqiang,ZHOU Hongwei et al. Joint Inversion of GPS and Gravity Data for Crustal
Movement in Fujian Area[J]. jgg, 2015, 35(1): 16-20.
