金竹山矿区测水组低硫煤成因机理研究  

RESEARCH ABOUT GENESIS PRINCIPLE OF LOW-SULPHAR COAL IN CESHUL FORMATION IN JINZHOUSHAN MINING DISTRICT

作　　者：杨荣丰[1] 莫时旭[1] 周新平 

机构地区：[1]湘潭矿业学院

出　　处：《东北煤炭技术》1996年第6期54-57,共4页

摘　　要：测水组是金竹山矿区的重要含煤地层，形成于泻湖－潮坪环境，煤层含硫低，主要与海水淡化、沉积环境及顶板岩相有关。Ceshui formation is the main coal-bearing strata in Jinzhoushan Mining district,which formed in cogoon-tidal falt circumtance and mainly related with desalination of sea water,deposition circumtance and roof rock-facies. The coal contaained in the formation has low sul-phar.

关 键 词：测水组 低硫煤 煤矿床 成因机理 

分 类 号：P618.110.1[天文地球—矿床学]