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《Progress in Geophysics》 2014-01
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The crust velocity structure of Da Hinggan Ling orgenic belt and the basins on both sides

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;  
Xinbaerhu-Qiqihaer Deep Seismic Sounding profile is about 630 km long,which goes across Hailaer basin.Da Hinggan Ling orgenic belt and Songliao basin.According to travel-lime data of 5 seismic phases and the amplitude information which were recognized by the recorded sections in 9shots.the authors obtained the two-dimensional P waves velocity structure along the profile,the thickness of crust is about 39.0?41.0 km in Hailaer basin,the thickness of crust from 38.5?43.5 km in the west to 34.5?36.4 km in the east of Da Hinggan Ling orgenic belt,the thickness of crust is about32.4?36.2 km in Songliao basin,analyzed the difference structure of crust and upper mantle of Da Hinggan Ling orgenic belt and the basins on both side,lo discuss the relation of basin-mountain structure..
【Fund】: 国家地质调查项目(1212011120975)《松辽盆地-大兴安岭-海拉尔盆地岩石圈精细结构调查与资源远景》资助
【CateGory Index】: P542
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