煤炭工程 ›› 2016, Vol. 48 ›› Issue (4): 100-103.doi: 10.11799/ce201604030

• 研究探讨 • 上一篇    下一篇

阳关寨整装勘查区含煤地层沉积环境及聚煤特征研究

黄文,熊炜   

  1. 贵州省煤田地质局地质勘察研究院
  • 收稿日期:2015-07-02 修回日期:2015-08-12 出版日期:2016-04-10 发布日期:2016-04-18
  • 通讯作者: 黄文 E-mail:67147929@qq.com

Features of coal bearing strata sedimentary environment and coal accumulation in Weining county Yangguanzhai integrated exploration area

  • Received:2015-07-02 Revised:2015-08-12 Online:2016-04-10 Published:2016-04-18

摘要: 根据含煤地层的单井岩性、沉积构造以及煤岩煤质特点,对贵州省威宁县阳关寨背斜整装勘查区宣威组进行了沉积特征、沉积序列、沉积环境和聚煤规律分析,结果表明:研究区宣威组以16号煤层为界,可分为曲流河河道和河岸沉积以及曲流河洪泛盆地沉积两种聚煤环境,聚煤作用主要发生在16号煤层底界—煤系顶界的曲流河洪泛盆地沉积环境,形成的煤层厚度较稳定~稳定,分布范围较广,为区内具有工业价值的主要煤层。

关键词: 整装勘查区, 宣威组, 煤系地层, 沉积环境, 聚煤规律

Abstract: With exploring the Yangguanzhai integrated exploration area and the analysis on the great borehole in formation, with the basic theory and method of the sedimentary、petrology and coalfield geology, the paper analyzed the sedimentary features、sedimentary sequences and sedimentary environment of the coal bearing strata in Weining county Yangguanzhai integrated exploration area., the paper had a study on the coal accumulation law,The results showed that the coal bearing strata of under segment Xuanwei formation in Yangguanzhai integrated exploration area is formed by meandering river flood basin sedimentary environment, the Characteristic of coal bed is lower continuity, small thickness, bifurcation, also ofen appeared pinch-out phenomenon; upper segment of Xuanwei formation is formed by meandering river and the bench sedimentary environment,the Characteristics of coal bed is good continuity, small thickness, good stability, simple structure of coal seam.

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