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《Chinese Journal of Geophysics》 2014-02
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Crustal structure of the northern margin of north China craton from Huailai to Sonid Youqi profile

LI Wen-Hui;GAO Rui;Keller Randy;LI Qiu-Sheng;HOU He-Sheng;LI Ying-Kang;ZHANG Shi-Hong;Key Laboratory of Earthprobe and Geodynamics,Ministry of Land and Resources;Lithosphere Research Centre,Institute of Geology,Chinese Academy of Geological Sciences;The University of Oklahoma;Core and Samples Center of Land and Resources;China University of Geosciences(Beijing);  
The SinoProbe-02 North China joint seismic experiment consisted of three seismicrecording efforts along 453km long profile.The profile extended from the Huailai basin,across the Yinshan-Yanshan belt,Inner Mongolia paleo-uplift,Bainaimiao arc,Ondor Sum accretion complex to the Solonker suture zone.We processed,analyzed,and modeled the data collected during the wide-angle reflection and refraction effort.The seismic waves from 8explosions were recorded by 300Texan recorders.The P-wave field provided good quality data for most of the profile.Arrivals of refracted and reflected waves from sediments and basement(Pg),intracrustal phases(PcP,PlP),and the Moho(PmP,Pn)were typically observed.Hole′s first arrival tomography program was used to obtain the upper crustal velocity structure.And Zelt′s 2Dtravel time raytracing and inversion program(Rayinvr)was used to obtain the full crustal structure.The final 2DP-wave velocity model contains many features of tectonic significance:(1)The flat and relatively shallow Moho in the Central Asia Orogeny Belt(CAOB)may be attributed to the extension;thicker crust appears beneath the Yinshan-Yanshan belt and was probably generated by compression in the Jurassic-Cretaceous and modified during the later extension;(2)The velocity structure varies significantly from the NCC to the CAOB,and the boundary between them appears at the Chifeng-Bayan Obo fault;(3)Relatively high velocities in the upper crust of the middle part of the profile may represent the outcrop of large area granites;strong velocity variations beneath the Bainaimiao arc and Ondor Sum subduction accretion complex indicate that multiple pulses of magmatism occurred during the complex tectonic evolution of this area.
【Fund】: 国家专项项目“深部探测技术实验与集成”(SinoProbe-02);; 国家自然科学基金(40830316、41274097、41104060);; 中国地质调查局地质调查项目(1212011120975、1212011220260)联合资助
【CateGory Index】: P313
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