摘要
This paper discusses the response relationship between sedimentary basin prototype of the NCC (North China Craton) and the early tectonic deformation of Craton destruction. During Late Triassic, the results show that: 1) the Upper Triassic Yanchang Formation develops well in the Ordos Basin, the center of the NCC, and it extended eastward to central Shanxi and western Henan areas; 2) the Upper Triassic Xingshikou Formation on the northern margin of the craton distributed sporadically along the line of western Liaoning—western Beijing—northern Hebei Province; and 3) on southern margin of the craton, the Upper Triassic developed in the northern Qinling area, along the line of southern Henan-Southern Shaanxi Province.