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《Chinese Journal of Geophysics》 2014-02
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Crustal velocity structure from the northern margin of the North China Craton to the southern margin of the Siberian plate

LI Ying-Kang;GAO Rui;YAO Yu-Tao;MI Sheng-Xin;LI Wen-Hui;XIONG Xiao-Song;GAO Jian-Wei;Geological Information Centre,Ministry of Land and Resource;Institute of Geology,Chinese Academy of Geological Sciences;  
Deep Seismic Sounding profile from Zhangjiakou to China-Mongolia border is about 600km long,it goes across North China Plate,Xingganling-Mongolian orogenic belt and the Siberian plate.The recording of seismic waves from 8explosions was conducted of 300recorders along seismic line.The P-wave field provided good quality data for most of the profile.The authorsprocessed,analyzed,and modeled the data which was collected during the wide-angle reflection and refraction effort.There are six phases,arrivals of refracted and reflected waves from sediments and basement(Pg),the reflected wave form the bottom of upper crust(P2),in middle crust(P3),the bottom of middle crust(P4),in the lower crust(P5,only appears in the beneath Xianghuang-Sunite)and Moho(Pm).Crustal velocity structure was obtained by seismic dynamics ray method(seis88).The results show that,(1)In the upper crust where is in area between North China Plate and Mongolia orogenic belt and in area between Mongolia orogenic belt and the Siberian plate,there are obvious high-velocity partial variations,and a lot of Paleozoic granite and ultramafic rock are exposed in the ground surface.(2)The velocities which is 6.3~6.7km/s in the lower crust of southern margin of the North China Plate is higher than the velocities which is 6.1~6.7km/s in the lower crust of the northern margin of the Siberian Plate,and the interface of the southern margin of the North China Plate is more gently than the northern margin of the Siberian Plate.The reason is that,in Inner Mongolia orogenic belt,the violent undulation interface of middle and lower crust may be caused by the crustal shortening and orogenic uplift,the flatten and material exchange in different blocks of land and sea result in the different regions of the velocity heterogeneity.Moho is more gently in the south of F2fault and in the north of F4fault,which is 40~42km.There are double Moho boundaries between F2and F4fault,the No.1Moho uplifts obviously,the depth is 33.5km and velocities is 6.6to 6.7km/s.The No.2Moho lies low obviously,the deepest area reaches 47km in the beneath of F3fault and the velocity is 6.8to 6.9km/s,which was caused by the crust-mantle mixed substance.Based on the characteristics of the Moho,the authors consider that the south area of double Moho boundaries is the northern margin of the North China Plate,and the north area of double Moho boundaries is the southern margin of the Siberian plate,the split position of the North China Plate and Siberian plate is between F2and F4fault.
【Fund】: 深部探测技术与集成项目(Sinoprobe-02)资助
【CateGory Index】: P313
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