古地理学报 ›› 2021, Vol. 23 ›› Issue (3): 489-506. doi: 10.7605/gdlxb.2021.03.036

• 岩相古地理学及沉积学 • 上一篇    下一篇

岩相古地理优势相方法及应用——兼谈“广义”与“狭义”岩相古地理及若干新的研究方向*

李增学1, 李莹2, 刘海燕1, 王东东1, 王平丽1, 宋广增3, 李晓静1, 贾强1, 赵洪刚1   

  1. 1 山东科技大学山东省沉积成矿作用与沉积矿产重点实验室,山东青岛 266590;
    2 山东交通学院交通土建工程学院,山东济南 250357;
    3 济南大学水利与环境学院,山东济南 250022
  • 收稿日期:2020-11-09 修回日期:2021-01-15 出版日期:2021-06-01 发布日期:2021-05-25
  • 作者简介:李增学,男,1954年生,教授,1995年毕业于中国地质大学(北京),获博士学位,主要从事能源沉积学、岩相古地理学与煤地质学教学与研究。E-mail: lizengxue@126.com。
  • 基金资助:
    *国家自然科学基金项目(编号: 42072188,41872172,41672096)资助

Method and application of lithofacies palaeogeographic dominant facies: also discuss the lithofacies palaeogeography in broad and narrow sense and some new research directions

Li Zeng-Xue1, Li Ying2, Liu Hai-Yan1, Wang Dong-Dong1, Wang Ping-Li1, Song Guang-Zeng3, Li Xiao-Jing1, Jia Qiang1, Zhao Hong-Gang1   

  1. 1 Shandong Provincial Key Laboratory of Depositional Mineralization & Sedimentary Mineral, Shandong University of Science and Technology,Shandong Qingdao 266590,China;
    2 Shandong Jiaotong University,School of Water Conservancy and Environment,Jinan 250357,China;
    3 School of Water Conservancy and Environment,University of Jinan,Jinan 250022,China
  • Received:2020-11-09 Revised:2021-01-15 Online:2021-06-01 Published:2021-05-25
  • About author:Li Zeng-Xue,born in 1954,obtained his Ph.D. degree from Beijing Graduate School of CUGB in 1995,and is currently leading an active group working on energy sedimentology and sequence stratigraphy of coal basins in China.E-mail: lizengxue@126.com.
  • Supported by:
    National Natural Science Foundation of China(Nos.42072188,41872172,41672096)

摘要: 提出岩相古地理研究的优势相思路与方法,优势相划分由等时性界面限定的沉积持续时间和沉积厚度这条主线串联起来。优势相分析具有定性与定量兼有的特征,即以各种定性与定量的、反映某个时期或阶段沉积环境特点的关键因素或指标资料为基础,由点到线、由线到面,点、线、面结合,由二维到三维空间,确定该阶段或该时期占优势的主导沉积相或岩相。主导沉积相或岩相既要满足沉积持续时间的主导、又要满足沉积物质表现优势,还需满足盆地或区块总体背景和环境格局上的合理性与综合性。指出优势因素(或称优势参数)是优势相确定的基础和前提。提出了“广义岩相古地理”和“狭义岩相古地理”2个概念,在其研究内容、精度、理论深度、研究区域范围和应用等方面进行区别,但并不能由一两个指标就简单区分,需要综合对比和分析才可以界定。论文还论述了岩相古地理研究出现的7个新方向,这些新的研究方向可根据研究目的和解决的实际勘探目标,进行广义和狭义岩相古地理分析。运用优势相分析思路和方法,在柴达木盆地新生代等时性地层划分及建立了盆地等时地层格架基础上,进行了柴达木盆地关键时期岩相古地理恢复。

关键词: 优势相方法, 优势因素, 主导指标, 广义岩相古地理, 狭义岩相古地理, 柴达木盆地

Abstract: This paper puts forward the idea and method of dominant facies in the research of lithofacies palaeogeography. The dominant facies division is connected by the depositional duration and depositional thickness,which are confined by isochronous interface. The dominant facies analysis shows both qualitative and quantitative characteristics. In other words,based on various qualitative and quantitative key factors or index data that reflect the characteristics of sedimentary environment in a certain period or stage,using the workflow from point to line,line to plane,two dimensions to three dimensions,the dominant sedimentary facies or lithofacies of the aimed stage or period are determined. The dominant sedimentary facies or lithofacies should provide the dominance of sedimentary duration,show the superiority of sedimentary material expression,and demonstrate the rationality and comprehensiveness of the overall background and environmental pattern of the basin or block. It is pointed out that the dominant factor(or the dominant parameter)is the basis and premise of determining the dominant facies. In this paper,concepts of lithofacies palaeogeography are divided into the broad sense and the narrow sense which are based on the aspects of research content,accuracy,theory depth,research area and application. However,the differences between these two concepts can only be distinguished by comprehensive comparison and analysis,rather than by one or two indicators. This paper also discusses seven newly emerged directions of lithofacies palaeogeography research,such as sequence stratigraphy-lithofacies palaeogeography,tectonic-lithofacies palaeogeography,quantitative lithofacies palaeogeography,biology-lithofacies palaeogeography,coal forming lithofacies palaeogeography,reservoir lithofacies palaeogeography,etc.,which show distinctive characteristics and are an important development of lithofacies palaeogeography. These new research directions can be used to analyze lithofacies palaeogeography in both broad and narrow sense according to the research purpose and the actual exploration target. Based on the division of Cenozoic isochronous strata and the establishment of isochronous stratigraphic framework,the lithofacies palaeogeography of Qaidam Basin in the key period has been restored by using the idea and method of dominant facies analysis.

Key words: method of dominant facies, advantage factor, dominant parameter, lithofacies palaeogeography in broad sense, lithofacies palaeogeography in narrow sense, Qaidam Basin

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