石油与天然气地质 ›› 2020, Vol. 41 ›› Issue (4): 673-683.doi: 10.11743/ogg20200402
收稿日期:
2019-02-25
出版日期:
2020-08-01
发布日期:
2020-08-11
作者简介:
郭旭升(1965-),男,博士、中国工程院院士,石油地质综合研究和勘探。E-mail:基金资助:
Xusheng Guo(), Dongfeng Hu, Renchun Huang, Jinbao Duan, Zhili Jiang, Xiang Zhu
Received:
2019-02-25
Online:
2020-08-01
Published:
2020-08-11
摘要:
四川盆地东北缘米仓山前带胡家坝灯影组古油藏主要分布于灯影组四段,越靠近顶部丰度越高,储层沥青主要为油层沥青和运移沥青。油源对比分析表明,胡家坝灯影组古油藏油气主要来自于侧向的优质筇竹寺组烃源岩,不排除灯影组三段泥质烃源岩供烃的可能。川东北地区筇竹寺组烃源岩在晚志留世进入初期生油阶段;在二叠纪末进入生油高峰,此时油气侧向运移至胡家坝灯影组储层中形成古油藏;在中三叠世有机质演化进入高成熟阶段,古油藏中原油裂解;晚白垩世至今,构造抬升剥蚀使得古油藏遭到破坏,形成现今残留古油藏。胡家坝灯影组古油藏的发现对四川盆地震旦系灯影组油气勘探有重大意义。灯影组四段主要为一套台缘丘滩相沉积,优质储层发育,以一、二类储层为主,灯影组四段上覆筇竹寺组作为区域和直接盖层,封盖条件好,表明川东北地区震旦系灯影组具有较好的勘探潜力。
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