张严;罗顺社;吕奇奇;王铜山;詹贵斌;

• 1:长江大学地球科学学院

• 2:中国石油大学(北京)油气资源与探测国家重点实验室

• 3:长江大学油气资源与勘探技术教育部重点实验室

• 4:长江大学非常规油气湖北省协同创新中心

摘要(Abstract)：

为建立山西永济中条山地区汝阳群层序地层格架,分析沉积特征和演化规律,建立沉积模式;根据野外露头剖面观察与实测资料、铸体薄片资料及露头层序界面的识别,利用沉积学理论研究汝阳群沉积环境和层序特征,阐述各层序的相互关系及海平面变化特征。结果表明:山西永济中条山地区汝阳群为障壁型海岸陆源碎屑岩沉积体系、碎屑岩和碳酸盐岩混合沉积体系,发育障壁型海岸相、混积滨岸相、浅海陆棚相3种沉积相类型,识别3种亚相及6种微相;汝阳群划分为6个三级层序,体系域由海侵体系域和高位体系域组成;白草坪组和北大尖组沉积体系分布受控于物源和相对海平面的变化;发育碎屑岩障壁型海岸沉积和混合沉积两种相模式。

关键词(KeyWords)：华北克拉通;中条山地区;中—新元古界;汝阳群;沉积相;层序地层

Abstract:

Keywords:

基金项目(Foundation):国家科技重大专项(2016ZX05004-001);; 油气资源与探测国家重点实验室开放课题(PRP/open-1804)

作者(Author):张严;罗顺社;吕奇奇;王铜山;詹贵斌;

Email:

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