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沁水盆地安泽地区煤层气富集主控地质因素

侯月华 姚艳斌 钟林华 陈龙伟 陈杨 黄赛鹏

煤田地质与勘探2017,Vol.45Issue(6):60-65,71,7.
煤田地质与勘探2017,Vol.45Issue(6):60-65,71,7.DOI:10.3969/j.issn.1001-1986.2017.06.010

沁水盆地安泽地区煤层气富集主控地质因素

Factors affecting coalbed methane enrichment in Anze area,southeastern Qinshui basin

侯月华 1姚艳斌 1钟林华 2陈龙伟 3陈杨 4黄赛鹏1

作者信息

  • 1. 中国地质大学(北京)煤层气国家工程中心煤储层实验室能源学院,北京100083
  • 2. 兖州煤业股份有限公司,山东济宁273500
  • 3. 中国石油华北油田公司 河北任丘062552
  • 4. 中国地质图书馆,北京100083
  • 折叠

摘要

Abstract

Through deepened analysis of CBM geological conditions and reservoir conditions in Anze block,the CBM enrichment law and its major influencing factors were discussed.The results show that coal petrology and structure of coal seam,as well as lithological characteristics of roof and floor rocks of coal seam are three key factors influencing gas content.Generally,gas content was manly controlled by coal rank.The higher coal metamorphic degree resulted in higher adsorption capacity of coal,and thus the greater gas content.Locally,gas content is also influenced by buried depth of coal,faults,folds and lithology of seam roof and floor.In structurally gentle zone,CBM content increased with burial depth.In faulting zone,gas content in the upthrow side of normal fault was obviously lower than that in the downthrown side.CBM dispersed obviously through faults.Mudstone and shale roof and floor of coal seam show better sealing capacity than that of sandstone roof and floor.

关键词

煤层气富集/煤阶/断层/褶皱/顶底板岩性/安泽区块

Key words

CBM enrichment/coal rank/fault/fold/lithology roof and floor of the coal seam/Anze block

分类

能源科技

引用本文复制引用

侯月华,姚艳斌,钟林华,陈龙伟,陈杨,黄赛鹏..沁水盆地安泽地区煤层气富集主控地质因素[J].煤田地质与勘探,2017,45(6):60-65,71,7.

基金项目

国家自然科学基金项目(41472137) (41472137)

全国优秀博士学位论文作者专著资金(201253) (201253)

山西省煤基重点科技攻关项目(MQ2014-01)National Natural Science Foundation of China(41472137) (MQ2014-01)

A Foundation for the Author of National Excellent Doctoral Dissertation of PR.China(201253) (201253)

Coal Base in Shanxi Province Key Scientific Research Project(MQ2014-01) (MQ2014-01)

煤田地质与勘探

OA北大核心CSCDCSTPCD

1001-1986

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