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《Chinese Journal of Geophysics》 2017-05
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A traveltime tomography study by teleseismic S wave data in the northeastern part of North China Craton

HU Gang;TENG Ji-Wen;HE Zheng-Qin;DING Zhi-Feng;Institute of Geology and Geophysics,Chinese Academy of Science;University of Chinese Academy of Science;Institute of Geophysics,China Earthquake Administration;  
Seismic body wave tomography is one of the effective methods to reveal the crustmantle velocity structure. A large number of seismic wave imaging studies have been conducted in the North China Craton, in order to study the formation and evolution of the Craton, and provided important deep information. In this paper the waveform data recorded by 190 sets of broadband seismometers of the North China Earthquake Science array in October 2006-March2009 from the teleseismic events in epicenter range 30°~90° were used,after extracting 9105 S wave travel time residual data with the waveform cross-correlation method, to determine the Swave velocity structure of the study area from the surface to a depth of 600 km by the FMTT body wave tomographic inversion method.All seismic stations are consistent with each other, the teleseismic events are evenly distributed with a very good back-azimuthal coverage, which allows us to get a higher resolution S wave structure than existing seismic body wave tomography result, and it can well reveal the deep crust and mantle structure and the dynamic mechanism of the study area, and provide new deep information for the major research project of North China craton lithospheric thinning and destruction. The conclusions are as follows:(1) The low velocity anomaly in Shanxi rift in the western part of the study area extends from the surface to the depth of the mantle transition zone at about 300 km, this reflects that hot materials exist beneath Shanxi rift. It is found that the low velocity anomaly does not penetrate the mantle transition zone to reach the lower mantle; it is speculated that the low velocity anomaly may be associated with the formation of the Mesozoic to Cenozoic Datong volcanoes and the upwelling of asthenosphere substance.(2) Regional seismic tomography study found that the leading edge of the Pacific Plate subduction has arrived at approximately 120°E(Huang and Zhao, 2006). We find that a high velocity anomaly extends from the crust of the Bozhong depression west-and down-wards to the mantle transition zone near 410 km beneath the Taihang piedmont fault, it is speculated to be the westward subducting Pacific plate in the mantle transition zone beneath eastern North China Craton.(3) Compared with the old cratonic lithosphere thickness the lithosphere of North China has been thinned, showing the complex phenomenon of alternating high and low velocities within the North China Plain, while the Yanshan region shows high-speed anomalies, indicating that the North China Plain lithosphere beneath the region has undergone significant erosion and destruction, and in the Yanshan region no significant erosion and destruction took place.
【Fund】: 基本科研业务费专项“太原盆地浅层速度结构探测(DQJB14C04)”;; 科技部科技基础性工作专项”华北地下精细结构探查”(2006FYll0100)联合资助
【CateGory Index】: P315.31
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【Citations】
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