Oil and gas migration and their reservoir formation in Lixian Slope are controlled by the nose-like struc-tural belts mainly resulted from the inherited development and later-period differential compaction against the back- ground of the uplift of the basement. The belts are characterized by eontinous development and episodic evolution, which are divided into 4 stages, namely Basement-Es4, Es3-ESlX, Es1sand Ed. This kind of characteristic has 3 kinds of controlling actions to the hydrocarbon accumulation: the development periods and times control the formation of overlying pinchout-type sandbodies along the two wings, the later nose-like structural crest makes channel len-shaped sandbodies developed; tong-existed structural peak dominates the petroleum migration and results in the formation of the following oil reservoirs : faulted nose, updip pinehout, sandstone lens and structural lithologic one ; the latter is the most popular type of the oil reservoir on Lixian Slope.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址:北京市海淀区学院路29号 邮编:100083 电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700 |