岩性油气藏 ›› 2023, Vol. 35 ›› Issue (2): 5967.doi: 10.12108/yxyqc.20230206
郑彬1, 董翱1, 张源智2, 张毅1, 苏珊3, 张士超1, 樊津津1, 骆垠山2
ZHENG Bin1, DONG Ao1, ZHANG Yuanzhi2, ZHANG Yi1, SU Shan3, ZHANG Shichao1, FAN Jinjin1, LUO Yinshan2
摘要: 通过对济阳坳陷渤南洼陷古近系沙河街组泥页岩和致密砂岩中的流体包裹体进行古压力测试,恢复了其流体压力演化过程,并探讨了其石油地质意义。研究结果表明: ①渤南洼陷沙三段在馆陶组沉积期及之后共经历了4次压力场重建过程,每次压力场重建的持续时间均为3~4 Ma,表现为低序级幕式特征。②与沙三段低序级幕式压力建场过程不同的是,沙四上亚段在上覆石膏岩的封盖下,压力场重建的门限较高,在东营组沉积期及馆陶组沉积末期发生2次压力场重建过程,表现为高序级幕式特点。③研究区沙三段低序级幕式压力建场过程指示着开放的流体环境和较强的酸性溶蚀作用,以低序级幕式压力建场为主的沙三段储集层物性整体优于高序级幕式建场的沙四上亚段储集层;沙三段烃源岩在排出大量烃类物质的同时,其自身储集空间中也会存在部分残留,从而形成常规油与页岩油的共同富集区。
中图分类号:
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