Three-dimensional crustal velocity structure model of the middle-eastern north China Craton （HBCrust1.0）

• Published in: 中国科学：地球科学英文版 2016 (7), p.1477-1488
• Main Author: DUAN YongHong WANG FuYun ZHANG XianKang LIN JiYan LIU Zhi LIU BaoFeng YANG ZhuoXin GUO WenBin WEI YunHao
• Format: Article
• Language: English
• Subjects: 三维速度; 华北克拉通; 唐山地震; 地壳速度; 宽角反射/折射; 岩浆底侵作用; 平均速度; 结构模型
• ISSN: 1674-7313; 1869-1897

Lithosphere thinning and destruction in the middle-eastern North China Craton（NCC）, a region susceptible to strong earthquakes, is one of the research hotspots in solid earth science. All 42 seismic wide-angle reflection/refraction profiles have been completed in the middle-eastern NCC. We collect all the 2-D profiling results and perform gridding of the velocity and interface depth data, building a 3-D crustal velocity structure model for the middle-eastern NCC, named HBCrust1.0, by using the Kriging interpolation method. Our result shows that the first-arrival times calculated by HBCust1.0 fit well with the observations. The result demonstrates that the upper crust is the main seismogenic layer, and the brittle-ductile transition occurs at depths near interface C（the interface between upper and lower crust）. The depth of interface Moho varies beneath the source area of the Tangshan earthquake, and a low-velocity structure is found to extend from the source area to the lower crust. Based on these observations, it can be inferred that stress accumulation responsible for the Tangshan earthquake may have been closely related to the migration and deformation of the mantle materials. Comparisons of the average velocities of the whole crust, the upper and the lower crust show that the average velocity of the lower crust under the central part of the North China Basin（NCB） in the east of the craton is obviously higher than the regional average. This high-velocity probably results from long-term underplating of the mantle magma.