岩性油气藏 ›› 2024, Vol. 36 ›› Issue (2): 4351.doi: 10.12108/yxyqc.20240205
包汉勇1, 刘皓天1, 陈绵琨1, 盛贤才1, 秦军1, 陈洁1, 陈凡卓2
BAO Hanyong1, LIU Haotian1, CHEN Miankun1, SHENG Xiancai1, QIN Jun1, CHEN Jie1, CHEN Fanzhuo2
摘要: 利用岩心、测井与地震资料,采用地震解释、平衡剖面以及包裹体检测等技术,恢复了川东地区高陡构造带的构造演化史,并对平桥、建南、梓里场构造的天然气来源、运聚与保存条件进行了分析。研究结果表明:①川东地区平桥断背斜圈闭东翼的单条逆断层使得下盘的龙马溪组烃源岩与上盘的洗象池群储层发生了侧向对接,天然气可穿过断裂带向上盘储层运移,具备较好的输导条件,且圈闭盖层未受到断裂作用破坏,保存条件良好,有利于天然气的聚集成藏。②建南断背斜圈闭翼部的多条平行的逆断层虽然实现了部分源-储对接,但是多条断层组合降低了其侧向输导能力,天然气未能大规模聚集。③梓里场断背斜圈闭的源-储配置与输导条件优良,但盖层的封盖能力较差,大多被断层破坏,钻探显示储层为水层。④川东地区高陡构造带寒武系洗象池群天然气聚集成藏的主控因素包括:断层或断层组合控制下的源-储配置、侧向输导条件以及盖层的封盖能力。
中图分类号:
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