Sedimentary Environment Analysis of Yingcheng Coalfield
详细信息   
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.

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