陈留勤,郭福生,梁伟

• 1:江西省核资源与环境重点实验室
• 2:中国地质科学院地质研究所
• 3:东华理工大学地球科学学院

摘要(Abstract)：

目前层序地层学研究多种模式并存,具备较为成熟的概念体系。理论和实践研究表明层序地层学理论可用于陆相地层分析。但是,由于海相和陆相地层与生俱来的明显差异,导致陆相层序地层研究更为复杂,需要更新的研究思路和更为有效的、精细的分析方法,所以陆相层序地层研究仍然是有待深入研究的一个领域。基于国内外陆相层序地层研究现状及存在问题,本文对陆相层序地层研究工作的基本原则、基准面和可容纳空间、陆相层序发育模式及体系域组成等核心内容进行了综述和探讨分析。在陆相层序地层研究工作过程中,需要重视露头和现代沉积的研究,融合测井和地震等地球物理资料,研究构造活动和古气候变化对层序地层结构的影响和控制作用,从成因上完善陆相层序地层模式、概念体系及工作流程。需要重视和加强河流泛滥平原细粒沉积的研究,古土壤不仅是良好的地层对比标志,同时也包含了重要的古气候信息。米兰科维奇天文旋回驱动在陆相和海相沉积地层中沉积响应的对比将有助于陆相高频层序的研究,因而具有重要意义。

关键词(KeyWords)： 层序地层;陆相地层;河流相;基准面;可容纳空间;体系域

Abstract:

Keywords:

基金项目(Foundation): 博士后科研启动基金项目(DHBHK1102);; 江西省博士后科研择优资助项目;; 江西省教育厅资助科研项目(GJJ13438);; 中国地质调查局工作项目(1212011120836);; 东华理工大学核资源与环境教育部重点实验室开放基金项目(NRE1210)

作者(Author): 陈留勤,郭福生,梁伟

DOI: 10.19839/j.cnki.dcxzz.2014.02.013

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