摘要
Objective The widely-distributed reformed basins in China are currently major areas for oil and gas exploration.Poststage tectonic movement of modified basins often plays an important role in controlling petroleum accumulation,migration and distribution(Liu and Yang,2000).The petroliferous Carboniferous-Permian Yingen-Ejinaqi Basin is located in the junction area between the North China Craton and the Central Asian Orogenic Belt(Fig.1 a).
基金
supported by the National Natural Science Foundation of China(grant No.41972153)
the Geological Survey project of the Chinese Geological Survey(grant No.DD20160172)。
