摘要
The Jiangnan-Xuefengshan mole track is a southeast to northwest and south to north basement detachable nappe. It formed during the Indosinian movement at the end of the Middle Triassic and compelled the Middle Paleozoic basin in south margin of the middle Yangtze region to produce a strong to weak deformation. In the front edge of the Xuefengshan nappe, a series of fault propagation anticline oil seepages developed from the Middle Paleozoic basin in the south margin of middle Yangtze region such as Cili Miaoshi, Chibi Beimencha, Jingshan Yanmenkou, and so on. The oil-source correlation indicates that these reservoirs accepted the mixed matters composed of surrounding rocks and hydrocarbon source rocks. This implicates that there may exist hydrocarbon source regions under the footwall of the thrust fault.