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《SEISMOLOGICAL RESEARCH OF NORTHEAST CHINA》 1999-01
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GEOLOGIC INTERPRETATION OF SEISMIC TOMOGRAPHIC IMAGE 3 KM DEPTH IN THE NORTHEAST EDGE OF SINO-KOREAN PLATFORM

Lei Qingqing; Meng Buzai; Niu Xue(Engineering Seismological Research Institute of Liaoning Plovince, Shenyang, 110121 )Lu Zaoxun(Seismological Bureau of Liaoning Province. Shenyang, 110031)  
Using rich geological and man-made seismic sounding data. the authors make a interpretationseismic tomographic image 3 km deep in the northeast edge of Sino-Korean platform. The results show that: 1. Thevelocity of 3km seismic tomographic image 3 km deep cosincide with the velocity of man-made seismic sounding.2. The velocity image of seismic tomographic inversion correspond good with the rock medium distribution at thesame depth : The high velocity area corresponds good with the medium distribution at same depth. The high velocityarea corrrespound with Archaeozoic-Lower Proterozoic Erathem metamorphic rocks and Palaeozoic Erathemmiddle-lower metamophic rocks of geosyncline. The Lower velocity area corresponds with Mesozoic Erathemvolcanic-clastic rock. Yanshanian Stage granite hody and Middle Proterozoic-Palaeozoic Erathem sedimentaryrocks as cover.3. The results of seismic tomographic image can provide basis for dividing rock unit of differentdepth and analysing a certain depth paleogeomophic face as wellas some structure unit.
【CateGory Index】: P315.63
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