Interpretation of S-Wave Data from Fanshi-Taipusiqi DSS Profile and Analysis of Correlation between Deep Structural Characteristics and Seismicity

查看全文 作　　者：Zhou Xuesong,Song Songyan,Zhang Xiankang,Qiu Shuyan,Gong Yi,and Song JianliResearch Center of Exploration Geophysics,SSB,Zhengzhou 450003,China 出　　处：《Earthquake Research in China》索引1998年第12卷第1期,共10页 摘　　要：By processing S-wave data from the Fanshi-Huai’an-Taipusiqi DSS profile,which is a three-component,wide-angle reflection/refraction profile,and in the light of the results from P-wave interpretation,two-dimensional(2-D)structures of the crust and upper mantle are presented,including S-wave velocity Vs and the physical parameter of medium-Poisson’s ratio a.Taking other geological and geophysical information into account,and with reference to the results from petrophysical experiments at home and abroad,we carried out interpretation and inference with respect to deep crustal structure,tectonics,and lithologic characters.It has been concluded that in the upper and middle crust,a values are mostly not greater than 0.25,and rocks,which generally assume brittle,are mainly composed of granite; the rocks in the lower layer of the upper crust between Yangyuan-Huai’an containing inorganic CO2 itself releases carbon; for the rocks in the lower crust and crust-mantle transitional zone,which are comparatively 关 键 词：S-WAVE velocity Poisson’s ratio lithologic character ultra-crustal fault earthquakes.