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《Crustal Deformation and Earthquake》 1986-01
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A PRELIMILARY INVESTIGATION FOR CRUSTAL VELOCITY-LAYER STRUCTURE USING EXPLOSION SEISMIC PROFILE FROM THE JIAJIAWAN TO THE SHAYUAN, HUBEI

Chen Buyun. Gao Wenhai (Institute Seismology, State Seismological Bureau)  
In this paper, the data obtained from Jiajiawan-Shayuan profile (about 471 km) among the four explosion seismic profiles set up on two sides of East-Qinling Structural Zone during 1979-1981 years are analyzed for recognition of several groups of P wave phases and synthetic inversion of the travel time of refraction and reflection wave with the broad sense linear inversion techniques. As a result, the velocity distribution in the crust and the upper mantle together with a model of the crust show that crust in this region is composed of layer inhomogeneous medium having a lower velocity layer and a thin layer with higher velocity within middle of the crust. The average velocities of P wave inthe crust and at the top of the upper mantle are 6.33 km/sec and 8.02 km/sec, respectively.The crust thickness is about 34.5 km within adistance of △≤200 km, but the crustal thickness gets up nearly 43 km within a distance of △≥280 km. There is a bulge of M-D beneath the section across the Yangzi River.
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