岩性油气藏 ›› 2023, Vol. 35 ›› Issue (6): 4553.doi: 10.12108/yxyqc.20230606
李恒萱, 温志新, 宋成鹏, 刘祚冬, 季天愚, 沈一平, 耿珂
LI Hengxuan, WEN Zhixin, SONG Chengpeng, LIU Zuodong, JI Tianyu, SHEN Yiping, GENG Ke
摘要: 被动大陆边缘盆地勘探程度低、潜力大,塞内加尔盆地是近年来被动陆缘勘探的热点地区之一。基于板块学说,利用地震、地质等资料,恢复了塞内加尔盆地的演化过程,并展望了其岩性油气藏勘探前景。研究结果表明:①塞内加尔盆地可划分为3个演化阶段,中三叠世裂陷期陆内裂谷盆地、晚三叠世—早侏罗世过渡期陆间裂谷盆地、中侏罗世至今漂移期被动陆缘盆地。受古构造和古气候的控制,裂谷层系较薄,且埋藏深,以陆相红色地层为主;陆间裂谷期广泛发育蒸发岩相;漂移期坳陷层序沉积厚度大,深水沉积体系是目前已发现油气田的重要储集层。②中部次盆深水区主要发育下白垩统阿尔布阶三角洲砂体,油气侧向或垂向运移形成下白垩统断层-岩性复合油气藏;超深水区发育上白垩统塞诺曼阶-马斯特里赫特阶浊积扇砂体,下部油气向上运移形成上白垩统海底扇岩性油气藏;毛里塔尼亚和卡萨芒斯盐盆主要发育中新统浊积扇砂体,盐底辟对油气运移和封闭具有重要影响,可形成与盐构造相关的油气藏。③通过已发现油气藏的成藏规律可预测尚未钻井的毛里塔尼亚、卡萨芒斯次盆可能也发育上白垩统海底扇岩性油气藏,且整个盆地陆架碳酸盐岩台地存在礁滩体油气藏,为下一步重点勘探领域。
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