摘要
Based on the analysis of structural tectonics and evolution,Jingzhou anticlinal belt of Jiangling Sag,which uplifted during the middle period of Jingsha Formation sedimentary,was a result of general effect of salt swell action,tectonic movement and volcanic event.An evident migration effect is observed by dissecting the oil pool in Jingzhou anticlinal belt.The oil measuresⅠ at the top of structure are mainly complex fault block,mostly controlled by faults,while the lithologic reservoirs of oil measures Ⅱ are mainly in southern ramp region and low-lying belt by sandstone reserve,controlled by sandstone reservoir.