吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (1): 52-64.doi: 10.13278/j.cnki.jjuese.20200140
• 地质与资源 • 上一篇
刘培, 张向涛, 林鹤鸣, 杜家元, 冯进, 陈维涛, 梁杰, 贾培蒙
Liu Pei, Zhang Xiangtao, Lin Heming, Du Jiayuan, Feng Jin, Chen Weitao, Liang Jie, Jia Peimeng
摘要: 西江主洼是珠江口盆地一个低勘探程度洼陷,油气差异聚集特征明显,但其机理不清。本文在断陷盆地油气成藏理论指导下,利用研究区地质、地球物理和地球化学等资料,开展了烃源岩、断盖组合、储集体系和运聚模式等方面的研究。结果表明,裂陷期沉降、沉积中心有序迁移,造成主力烃源岩自东向西由文四段迁移至文三段、文一+二段,控制东、西部油气差异分布。恩平组区域性泥岩发育且晚期断裂缺乏,导致油气纵向上更易聚集于下构造层;区域泥岩减薄尖灭或晚期断裂切开盖层的区域,上构造层有一定油气分布。"源-汇"类型从宏观上控制储层优劣,影响下构造层油气富集程度;"仓储"运移是控制上构造层油气规模聚集的主要模式。下构造层古近系应作为重点部署方向,东部围绕文四段、西部围绕文三段、文一+二段烃源岩构成的含油气系统展开;上构造层勘探需关注珠海组,在隆起周边寻找具备"仓储"运移模式的有利区带。
中图分类号:
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