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《Chinese Journal of Geophysics》 2008-01
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Relocation of earthquakes in Jiangsu and neighboring areas,China and analysis of structural features

HUANG Yun~ 1,2 ,LI Qing-He~2, ZHANG Yuan-Sheng~3, SUN Ye-Jun~2, SHEN Hong-Hui~2, JIN Shu-Mei~21 Institute of Geophysics, CEA, Beijing 100081, China2 Earthquake Administration of Jiangsu Province, Nanjing 210014, China3 Lanzhou Institute of Seismology, CEA, Lanzhou 730000, China  
The earthquakes happened in and around Jiangsu province from 1980 to 2005 were relocated precisely by using Double-Difference(DD) method and Genetic Algorithm(GA). The result shows that the earthquakes are more concentrated in some areas and the distribution of focal depth is more reasonable. Most earthquakes happened in the upper and middle crust. The distributions of focal depths are similar basically for Lower Yangtze Block, Hebei-Shandong Block and Henan-Anhui Block. There are two predominant depths: 10~11 km and 15~17 km, where more earthquakes happened. We infer that they are in the bottom of upper crust and in middle crust respectively. At 25 km, there is a minor predominant focal depth. In Dabie Orogenic Zone, most focal depths are less than 10 km, especially, concentrate in 6~7 km. Maybe there is high velocity in that depths. The shallower focal depth is the major feature of Dabie Orogenic Zone different from other tectonic provinces as mentioned above, but below 10 km they have similar features.
【Fund】: 国家自然科学基金(40374033)资助;; 地震联合基金(1040029)资助;; 江苏省科技发展项目(BS2003053)资助
【CateGory Index】: P315
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