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On the analysis of the high-resolution sequence stratigraphy and coal accumulating law of jurassic in Ordos Basin

机译:鄂尔多斯盆地侏罗系高分辨率层序地层及聚煤规律分析

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摘要

The strata of Jurassic was divided into three tectonic sequences and eight se-quences of third rank, according to the developing feature of the tectonic inconformity and the transforming feature of the depositional system tracts. Also the identification and the division of the base-level cycle of different period were carded through. Therefore three cycles of super period, eight cycles of long period, twenty-four cycles of middle period and some cycles of short pedod were identified. From the overall character of the coal-accu-mulation in the Mesozoic, we can see that the Yan'an formation is of the best nature of coal bearing. When the coal bearing systems of Jurassic were depositing, the Ordos area is the coal accumulating basin of terrene of large scale and located in the same tectonic unit. But the local structure of different part and the paleolandform are different in the basin,which resulted in the difference of the depositional environment. So the layer number and the distribution of the thickness of the coal beds are different in the different part of the ba-sin. The coal-accumulating action migrated regularly along with the development, evolve-ment and migration of the depositional systems. The layer numbers of the coal beds,which can be mined, are more in the north and west fringe of the basin, whose distributing area is extensive, and they are more steady in the landscape orientation, also the total thickness is great. Therefore the nature of coal bearing and the coal-accumulating action of different part changed obviously in the space in Ordos area.
机译:根据构造不整合面的发育特征和沉积系统道的转换特征,将侏罗纪地层划分为三个构造层序和八个层序。并梳理了不同时期基本周期的识别和划分。因此,确定了三个周期的超周期,八个周期的长期周期,二十四个周期的中期周期和一些短脚架周期。从中生代积煤的总体特征可以看出,延安组是含煤性最好的。当侏罗纪含煤体系沉积时,鄂尔多斯地区是大面积的特伦烯储煤盆地,位于同一构造单元中。但是该盆地不同部位的局部构造和古地貌不同,导致沉积环境的差异。因此,在盆地的不同部位煤层的层数和厚度分布是不同的。随着沉积系统的发展,演化和迁移,煤的蓄积作用有规律地迁移。可开采的煤层层数在盆地的北部和西部边缘较多,分布范围广,在横向上较稳定,总厚度也很大。因此,鄂尔多斯地区空间的含煤性质和不同部位的聚煤作用发生了明显变化。

著录项

  • 来源
    《煤炭学报:英文版》 |2008年第001期|85-91|共7页
  • 作者单位

    College of Geological Information Science and Engineering, Shandong University Sience Technology, Qingdao 266510,China;

    Research Center of Petroleum and Gas Exploration and Exploitation Techniques of Shandong, Qingdao 266510,China;

    College of Geological Information Science and Engineering, Shandong University Sience Technology, Qingdao 266510,China;

    Guangzhou Institute of Geochemistry Chinese Academy of Sciences, Guangzhou 510640, China;

    College of Geological Information Science and Engineering, Shandong University Sience Technology, Qingdao 266510,China;

    Research Center of Petroleum and Gas Exploration and Exploitation Techniques of Shandong, Qingdao 266510,China;

    College of Geological Information Science and Engineering, Shandong University Sience Technology, Qingdao 266510,China;

    Research Center of Petroleum and Gas Exploration and Exploitation Techniques of Shandong, Qingdao 266510,China;

    College of Geological Information Science and Engineering, Shandong University Sience Technology, Qingdao 266510,China;

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  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类 化学;
  • 关键词

    high resolution sequence stratigraphy, base-level cycle, coal accumulating law,the migration of rich-coal units;

    机译:高分辨率层序地层;基层旋回;聚煤规律;富煤单元运移;
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