陆相湖盆陆源碎屑与碳酸盐岩混合沉积研究进展  

Research Progress in Mixed Sedimentation of Terrigenous Clastic and Carbonate Rocks in Continental Lake Basins

作　　者：连旭欢 李俊宇 姜瑞海 张晨 崔云峰 

机构地区：[1]华北理工大学矿业工程学院,河北 唐山

出　　处：《地球科学前沿（汉斯）》2023年第9期1040-1050,共11页Advances in Geosciences

摘　　要：随着陆相湖盆非常规油气勘探取得重大突破,陆相湖盆陆源碎屑与碳酸盐岩混合沉积的产物作为致密油和页岩油重要的微观源储组合类型,逐渐引起了石油地质领域的高度重视。在前人研究的基础上,系统梳理、总结了国内外关于陆相湖盆陆源碎屑与碳酸盐岩混合沉积研究所取得的进展,详述了陆相混积的概念、成因机理、类型特征、混积模式、控制因素、油气地质意义等内容,旨在为陆相混积油气勘探开发提供地质依据。With significant breakthroughs in unconventional oil and gas exploration in continental lake ba-sins, the products of mixed sedimentation of terrigenous debris and carbonate rocks in continental lake basins, as important micro source and reservoir combinations of tight oil and shale oil, have gradually attracted high attention in the field of petroleum geology. On the basis of previous research, this paper systematically reviews and summarizes the progress made in the study of mixed sedimentation of terrigenous debris and carbonate rocks in continental lake basins at home and abroad. It elaborates on the concept, genetic mechanism, type characteristics, mixing mode, control factors, and geological significance of terrigenous mixing, aiming to provide geological basis for the exploration and development of terrigenous mixing oil and gas.

关 键 词：陆相湖盆 混合沉积 成因机理 混积模式 油气地质意义 

分 类 号：P61[天文地球—矿床学]