摘要
六盘水井田龙潭煤系为腐植煤类。宏观煤岩类型以半亮煤为主。无机显微组分以粘土矿物和石英为主。有机显微组分含量在69.20%~93.43%,以镜质组为主。最大镜质体反射率0.891%~1.930%,一般为中煤级煤Ⅲ~Ⅴ。此类煤层利于煤层气的富集高产。
The Longtan coal series in Liupanshui coalfield is humus coal.The macro coal type is mainly semi-bright coal.Inorganic microscopic components are mainly clay minerals and quartz.The content of organic micro-components ranges from 69.20%to 93.43%.The maximum reflectance of vitrinite is 0.891%~1.930%,which is generally medium coal grade coalⅢ~Ⅴ.Such coal seams are conducive to the enrichment and high production of coal seam gas.
作者
赵立鹏
钟方军
高为
周培明
Zhao Lipeng;Zhong Fangjun;Gao Wei;Zhou Peiming(Laboratory of Coalfield Geology Bureau of Guizhou Province,Guiyang 550008,China;Guizhou Coalbed Methane Shale Gas Engineering Technology Research Center,Guiyang 550008,China)
出处
《煤炭与化工》
CAS
2020年第3期49-50,80,共3页
Coal and Chemical Industry
基金
2018年度贵州省地勘基金项目“贵州省西部煤系气调查评价(GZMC-ZG20192014-1)”。
关键词
六盘水
龙潭煤系
煤岩
显微组分
Liupanshui
Longtan coal series
coal rock
microscopic composition