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EARTHQUAKE ›› 2018, Vol. 38 ›› Issue (4): 37-48.

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Upper Crust Velocity Structure Tomography of the Three Gorges Reservoir Area based on Dense Observation

ZHANG Na, ZHAO Cui-ping, Zhou Lian-Qing   

  1. Institute of Earthquake Forecasting, CEA, Beijing 100036, China
  • Received:2018-05-10 Published:2019-08-15

Abstract: In this paper, tomoDD method is applied to determine detailed 3D velocity structure of the upper crust and the hypocenter parameters simultaneously in the Three Gorges reservoir area using the phase arrival times from 4967 seismic events recorded by 48 instruments. The resolution of the inversion result is 0.05°. The following conclusions are drawn:The heterogeneity of medium is obvious, reflecting the complex media structure in the reservoir area. The VS distribution is bounded by the Xiangxi River between the Zigui Basin and the Huangling anticline. It shows a high VS distribution to the east of the Xiangxi River including the reservoir dam. To its west, there are obvious large-scale low VS distributions, including the Zigui basin, the Gaoqiao fault, and the Yangtze River. The distributions of low VP and VS in the Zigui Basin show that the sedimentary thickness of the basin is between 6 km and 8 km respectively. The low VS anomaly in the margins of the basin and Xiangxi River is significantly higher than VP, and fluid diffusion and infiltration may occur at the edge of the basin. The seismic events in the reservoir area, which clusted in the Badong area along the Yangtze River coast west of Xietan and the Xiannvshan area, forms a A-frame pattern, which is consistent with pervious observation. The lower boundary of focal depth is deeper from west to east with a dominant distribution between 0 and 10 km. The earthquakes along Gaoqiao fault in the Badong area occurred in the low or weak VS areas, implying the relationship between the occurrences of these earthquakes with the lithological conditions in this area. The December 2013 MS5.1 earthquake is located within a high VP and VS area and also at the bottom of a strip formed by shallow to deep earthquakes . The two M4 earthquakes in December 2016 located in the high VP and VS zone, the MS4.1 on March 27, 2014 and the MS4.7 earthquake on March 30, 2014 are located in the margin of high VP and VS areas as well.

Key words: Three Gorges reservoir area, tomoDD, 3D velocity structure, Seismic relocation

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