摘要
利用地质报告资料分析了五凤井田6含煤段沉积环境,探讨了首采区内6中煤薄煤带成因,认为6中煤薄煤带是由于砂体的冲刷作用形成的。
With the geological information, the sedimentary environment of NO. 6 coal - bearing section was analyzed and the causation of the NO. 6 thin - coal area were discussed. It＇ s thought that the NO. 6 thin -coal area was caused by flush effect of sand body.
出处
《贵州地质》
2008年第4期282-285,296,共5页
Guizhou Geology
关键词
五凤井田
6含煤段
沉积环境
薄煤带
成因分析
Wufeng orefield
NO. 6 coal - bearing section
sedimentary environment
thin - coal area
causation analyses
