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《Chinese Journal of Geophysics》 1985-05
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AN INTERPRETATION OF THE DSS DATA ON MENYUAN-PINGLING-WEINAN PROFILE IN WEST CHINA

ZHANG SHAO-QUAN WU LI-JUN GUO JJAN-MING CHEN XUE-BO ZHAO JING-XIAN DING YUN-YU HUANG CHANG-LIN ZHANG CHANG CHEN ZHI-TAI (The State Seismological Bureau)  
In order to study the deep structure in West China, a profile of deep seismic sounding (DSS) has been made by the State Seismologieal Bureau (SSB). This profile starts from Menyuan (门源) at its west end and to Weinan (渭南) at its east end. Total length is about 970 km.On the profile are 7 shooting points, constituting a continuous profiling of forward and reverse shooting. Based on kinematic and dynamic characteristics of waves, we can recognize a head wave from crystalling basement and three reflected waves from M-discontinuty and others. We have used several methods of interpretation, such as inversion by travel times, ray tracing and synthetic seismograms. We can divided the crust into four layers with the following structure parameters:H1= 03.32±1.01 km, V1 = 4.35±0.79 km/sec;H2 = 11.79±2.77 km, V2 = 6.06±0.24km/sec;H3 = 11.58±4.32 km, V3 = 6.35±0.26 km/sec;H4 = 17.64±7.25 km, V4 = 6.52±0.57 km/sec.The average thickness of the crust is 45.60±11.01 km.The results indicated that the crust in this region is laterally inhomogeous. The relieves of M-boundaries of the, west part of the profile are comparatively small, while those of the middle and east parts are larger. They seem to show a U-shaped structure which is wider in the upper part, and this is favouable to explain the geological tectonics and earthquake generation in this region.
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