• RSS
  • E-mail Alert
  • 收藏主页

古地理学报 ›› 2018, Vol. 20 ›› Issue (4): 623-636. doi: 10.7605/gdlxb.2018.04.045

• 岩相古地理学及沉积学 • 上一篇    下一篇

山西沁水盆地东北部太原组沉积序列及环境演化*

宋慧波1,3, 李亚南1, 于振峰2, 刘顺喜1, 胡斌1, 李紫源1   

  1. 1 河南理工大学资源环境学院,河南焦作 454003;
    2 煤与煤层气共采国家重点实验室,山西晋城 048200;
    3 中原经济区煤层(页岩)气河南省协同创新中心,河南焦作 454000
  • 收稿日期:2017-11-28 修回日期:2018-01-19 出版日期:2018-08-01 发布日期:2018-07-31
  • 通讯作者: 胡斌,男,1952年生,教授,博士生导师,主要从事古生物地层学、遗迹学和沉积学的教学和研究工作。E-mail: hub@hpu.edu.cn。
  • 作者简介:宋慧波,女,1979年生,副教授,博士,主要从事古生物地层学、遗迹学和沉积学的教学与研究工作。E-mail: songhuibo2005@hpu.edu.cn。
  • 基金资助:
    *国家自然科学基金项目(编号: 41772104)、河南省基础与前沿项目(编号:162300410256)、河南理工大学博士基金项目(编号: B2013-075)和山西省基础研究计划煤层气联合研究基金项目(编号: 2015012010)联合资助

Sedimentary succession and environment evolution of the Taiyuan Formation in northeastern Qinshui Basin, Shanxi Province

Song Hui-Bo1,3, Li Ya-Nan1, Yu Zhen-Feng2, Liu Shun-Xi1, Hu Bin1, Li Zi-Yuan1   

  1. 1 School of Resources and Environment,Henan Polytechnic University,Jiaozuo 454003,Henan;
    2 State Key Laboratory of Coal and Coalbed Methane Co-Mining,Jincheng 048200,Shanxi;
    3 Collaborative Innovation Center of Coalbed Methane and Shale Gas for Central Plains Economic Region of Henan Province,Jiaozuo 454000,Henan
  • Received:2017-11-28 Revised:2018-01-19 Online:2018-08-01 Published:2018-07-31
  • Contact: Hu Bin,born in 1952,is a professor and Ph.D. supervisor of Henan Polytechnic University. He is mainly engaged in teaching and researches of paleontology and stratigraphy,ichnology and sedimentology. E-mail: hub@hpu.edu.cn.
  • About author:Song Hui-Bo,born in 1979,is an associate professor with Ph.D. degree obtained from Henan Polytechnic University. She is mainly engaged in teaching and researches of paleontology and stratigraphy,ichnology and sedimentology. E-mail: songhuibo2005@hpu.edu.cn.
  • Supported by:
    Co-funded by the National Natural Science Foundation of China(No.41772104),the Basic and Frontiers Research Program of Henan Province(No.162300410256),the Doctoral Foundation of Henan Polytechnic University(No. B2013-075)and the CBM Union Foundation of Shanxi Province(No.2015012010)

RichHTML

PDF

摘要： 山西沁水盆地东北部上石炭统—下二叠统太原组含有丰富的煤与煤层气资源,在昔阳黑土岩村一带有良好的露头剖面。以黑土岩村剖面为主要研究对象,结合邻区部分钻孔资料,对石炭—二叠系太原组的岩石特征、沉积构造、化石组成及沉积序列类型进行了详细分析。取得如下成果: 在研究剖面中识别出有障壁和无障壁海岸以及三角洲3种沉积体系,5种沉积相、3种亚相和5种微相,并在太原组中部层段发现混积潮坪沉积;建立了9种沉积序列类型及其古环境分布模式,并基于沉积序列的垂向变化规律,提出了本区太原组的沉积环境模式,进而简要论述了太原组自下而上从障壁岛—潟湖—潮坪到浅海—潮坪,最后到三角洲的沉积环境演变过程。

关键词: 沁水盆地, 上石炭统-下二叠统, 太原组, 沉积相, 沉积环境

Abstract: The Upper Carboniferous-Lower Permian Taiyuan Formation in northeastern Qinshui Basin of Shanxi Province contains abundant coal and coalbed methane resources,and well outcrops in the area of Heituyan village in Xiyang County. Based on the researches of the outcrop section and some nearby exploration data,this paper detailedly analyzes the lithologic characteristics,sedimentary structures,fossil composition,carbonatite microfacies and sedimentary succession types of the formation and obtains the results as follows: Three kinds of sedimentary systems(including barrier shore,open shore and delta),five kinds of sedimentary facies,three kinds of sedimentary subfacies and five kinds of carbonate microfacies were recognized,and the mixed tidal flat deposits in the middle part of the Taiyuan Formation were found in this area. On this basis,nine types of sedimentary succession and their palaeoenvironment model were suggested. According to the vertical change tendency of sedimentary successions,this paper proposes the sedimentary environment model of the Taiyuan Formation and briefly discusses the evolution process of depositional environments,i.e.,from the bottom to top,ranging from barrier island-lagoon-tidal flat to shallow sea-tidal flat,and then to delta environments.

Key words: Qinshui Basin, Upper Carboniferous-Lower Permian, Taiyuan Formation, sedimentary facies, sedimentary environment

中图分类号: