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1. 中国地质大学(武汉) 资源学院
2. 成都理工大学沉积地质研究院
3. 中国地质大学(武汉)海洋学院
4. 中国石化勘探分公司物探研究院
5. 中国石油大学(华东)地球科学与技术学院
6. 中国地质大学(武汉)地质过程与矿产资源国家重点实验室
Published:2025
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邓空, 陆扬博, 张柏林, et al. 二叠纪中晚期地质事件对川东北富有机质页岩发育的控制[J]. Bulletin of Geological Science and Technology, 2025, 44(2): 161-181.
邓空, 陆扬博, 张柏林, et al. 二叠纪中晚期地质事件对川东北富有机质页岩发育的控制[J]. Bulletin of Geological Science and Technology, 2025, 44(2): 161-181. DOI: 10.19509/j.cnki.dzkq.tb20240483.
川东北地区二叠系大隆组、吴家坪组和茅口组中3套黑色富有机质页岩获页岩气勘探的重大发现,开辟了接替五峰组-龙一段海相页岩气勘探开发的新领域。基于岩石学、沉积学和地球化学分析,探讨了这3套黑色富有机质页岩的沉积特征及其沉积古环境的演化过程,综合分析了川东北地区二叠纪中晚期富有机质页岩沉积时期的古环境差异及有机质富集的控制因素。结果表明,茅口组、吴家坪组及大隆组富有机质页岩具有强烈的非均质性,其发育控制因素也存在显著差异。其中,茅口组三段沉积期受强上升流、弱火山和弱热液活动影响,气候温暖湿润,伴随有极高的初级生产力、低陆源输入及缺氧硫化的水体条件;吴家坪组二段所对应的沉积环境具备高生产力、低陆源输入、季节性上升流、弱热液活动及间隙硫化-硫化条件的特征;大隆组受强热液、上升流和岛弧火山的影响,其所对应的沉积环境具有高初级生产力、低陆源输入及间隙硫化-硫化条件的特征。研究结果进一步揭示了多重地质事件对富有机质页岩的复杂耦合作用,构建了多重地质事件联控的富有机质页岩成因模式,为海相页岩气勘探有利区提供了理论依据及模型支持。
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