天然气地质学

煤层在中国陆相盆地地层层序划分中的应用——以吐哈盆地红台地区中侏罗统为例

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  • 1.中国石油大学地球资源与信息学院 山东 东营 257061;
    2.中国石油新疆油田分公司勘探开发研究地球物理所,新疆 乌鲁木齐 830011

收稿日期: 2008-03-25

  修回日期: 2008-06-16

  网络出版日期: 2008-12-10

An Example of Coal Bed as the Stratigraphic Sequence Border in Continental Basin of China: Taking the Middle Jurassic of Hongtai Area, Tuha Basin for Example

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  • 1. School of Geo-Resources and Information, China University of Petroleum, Dongying 257061, China; 2. Institute of Geophysics, Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina,Urumqi 830011, China

Received date: 2008-03-25

  Revised date: 2008-06-16

  Online published: 2008-12-10

摘要

在国外成因地层学研究中早已提出将陆相盆地中区域性分布的煤层作为一种层序边界识别标志,为了验证该理论在中国陆相盆地地层层序划分中的适应性,特选择吐哈盆地红台地区进行研究。利用录井、测井、岩心、钻井等资料对红台地区地层划分和沉积相进行研究,研究层段主要为中侏罗统三间房组和七克台组,主要发育有湖泊相的滨浅湖亚相和辫状河三角洲相等沉积相类型。研究区内存在2期较为明显的低位煤层,各期煤层的发育均有旋回性特点,并且煤层中硅质碎屑含量也存在旋回性变化,所以煤层能够作为一种层序边界的识别和对比标志。利用煤层作为层序边界将目的层划分为2个半三级层序,在此基础上根据经典层序地层学理论和研究区目的层位的旋回性特征,将研究层段的层序细分至体系域。

本文引用格式

袁波,;陈世悦;夏雨 . 煤层在中国陆相盆地地层层序划分中的应用——以吐哈盆地红台地区中侏罗统为例[J]. 天然气地球科学, 2008 , 19(06) : 810 -815 . DOI: 10.11764/j.issn.1672-1926.2008.06.810

Abstract

The theory of the coal bed as the stratigraphic sequence border in a continental basin has been put forward abroad. For the purpose of combining this theory with the specific circumstances of the continental basin in China, we apply this theory to the study of the sequence stratigraphy in the Hongtai area, Tuha basin. We utilize the information about logging data, drill core and drilling data to analyze the division of lithostratigraphy and the sedimentary facies in the study area. The research formation is Sanjianfang Formation and Qiketai Formation in Middle Jurassic. And the main sedimentary facies are shore shallow lacustrine subfacies and braided river delta facies. There are two coal developing stages of LST in the study area, and each stage presents the cyclicity feature, the siliciclastic content in the coal bed also presents the cyclicity feature, so the coal bed as the stratigraphic sequence border in continental basin in China is feasible. Finally, we divide stratigraphic sequence in the work area, and the research formation is divided into two and half third order sequences.

参考文献

[1]邱荣华.层序地层学译文集[M].北京:石油工业出版社,1996:103-120.
[2]国景星,戴启德,吴丽艳,等.冲积河流相层序地层学研究[J].石油大学学报:自然科学版,2003,27(4):15-19.
[3]操应长,姜在兴,夏斌,等.利用测井资料识别层序地层界面的几种方法[J].石油大学学报:自然科学版,2003,27(2):23-26.
[4]彭立才,杨慧珠.柴达木盆地大煤沟侏罗系剖面高分辨率含煤层序分析[J].西安石油学院学报:自然科学版,2002,17(1):6-10.
[5]纪友亮,张世奇.层序地层学原理及层序成因机制模式[M].北京:地质出版社,1998:108-156.
[6]沈守文,彭大钧,颜其彬,等.层序地层学预测隐蔽油气藏的原理和方法[J].地球学报,2000,21(3):300-305.
[7]邵磊,李文厚,袁明生,等.吐鲁番—哈密盆地陆源碎屑沉积环境及物源分析[J].沉积学报,1999,17(3):435-441.
[8]李勇,邵磊.吐哈盆地侏罗系沉积特点及油气资源[J].西北大学学报:自然科学版,2004,34(6): 698-702.
[9]袁明生,牛仁杰,焦立新,等.吐哈盆地前陆冲断带地质特征及勘探成果[J].新疆石油地质,2002,23(5): 376-379.
[10]周丽清,吴胜和,熊琦华,等.吐哈盆地WM油田辫状河三角洲前缘砂体分析[J].沉积学报, 2000,18(2):248-252.
[11]刘海涛,卫延召,张光亚,等.准噶尔盆地白家海地区侏罗系聚煤作用与层序地层[J].天然气地球科学,2006,17(6):802-806.
[12]李红哲,杨占龙,吴青鹏,等.沉积相分析在岩性油气藏勘探中的应用——以吐哈盆地胜北洼陷中侏罗统—白垩系为例[J].天然气地球科学,2006,17(5):698-702.
[13]Frazier D E.Depositional Episodes:Their Relationship to the Quaternary Stratigraphic Framework in the Northwestern Portion of the Gulf Basin[R].Austin University of Texas:Bureau of Economic  Geological Circular 74-1,1974:1-28.
[14]李红哲,何琼英,吴青鹏,等.高分辨率层序地层学在吐哈盆地浅层中的应用[J].天然气地球科学,2006,17(1):102-105.
[15]Jervey M T.Quantitative geological modelling of siliciclastic rock sequences and their seismic expressions[C]//Wilgus C K.Sea-level Changes:An Integrated Approach,SEPM Special publication,1988,42:47-69.
[16]Tankard A J.Depositional response to foreland deformation in the Carboniferous of eastern Kentucky[J].AAPG,Bulletin 1986,70(7):853-868.

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