supported by Grants from National Natural Science Foundation of China(No.41172150);the Ministry of Land and Resources of China(No.201211005–1);China Geological Survey(CGS)(No.1212011120099);China Scholarship Council(CSC)
The Late Cenozoic basins in the Weihe-Shanxi Graben, North China Craton are delineated by northeast-striking faults. The faults have, since a long time, been related to the progressive uplift and northeastward expansi...