摘要
The authors studied the palaeotecctonic and coal accumulation,sedimentary environment of Yingcheng coalfield. The western margin of the basin Yinmahe fault(F2) is sloping plow-type fracture with NNE,SEE strike. Southeastern margin of the basin is falling home tension rupture(F1),which is numerous,splitted faulted basin formed by rifting of east of China Late Jurassic-Early Cretaceous period.