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
Ceshui formation,low-sulphar coal,genesis,Jinzhoushan
