孙蕗,邓成龙,郝青振,刘彩彩,易亮,刘平,高新勃,熊建国,杨石霞,葛俊逸

• 1:东华理工大学地球科学学院
• 2:中国科学院地质与地球物理研究所岩石圈演化国家重点实验室
• 3:中国科学院地质与地球物理研究所新生代地质与环境重点实验室
• 4:中国地震局地质研究所地震动力学国家重点实验室

摘要(Abstract)：

中国海相第四系主要沉积类型为碎屑沉积和生物礁沉积,陆相第四系岩性多变,相比已建立起高精度气候地层年代学标尺的海相地层来说,中国陆相第四纪地层尚未建立起统一的年代地层系统,这为地层的跨区域识别和对比带来了困难。解决这一科学问题的思路之一是针对陆相地层的岩性分布特征,分区域进行小规模、小范围的总结和推广。中国陆相更新统自下而上包括下更新统泥河湾阶、中更新统周口店阶和上更新统萨拉乌苏阶,全新统待建阶。本文在这个地层划分框架的指导下,将中国第四纪陆相地层分为黄土-古土壤序列、沙漠戈壁、网纹红土、河湖相和山麓堆积、洞穴/裂隙堆积及其他类型岩石地层几大类,海相地层按照碎屑沉积和生物礁沉积划分,并在每一类地层单元下遵循岩性组合、地貌类型和构造背景相似的原则进行归纳,分区域探讨并总结近年来与其相关的代表性研究进展,为早日建立统一的陆相第四系年代地层系统贡献力量。

关键词(KeyWords)： 岩石地层;地层分区;划分和对比;第四系;年代地层学;磁性地层学;中国

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金(41690112、41888101、41504058);; 东华理工大学博士科研启动基金(DHBK2019049)共同资助

作者(Author): 孙蕗,邓成龙,郝青振,刘彩彩,易亮,刘平,高新勃,熊建国,杨石霞,葛俊逸

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