摘要
通过对以往钻孔、勘查成果、成煤环境、煤层厚度变化规律的研究,认为该区煤炭资源形成于陆相三角洲平原,主要控煤因素是三角洲平原上发育的分支河道沉积。分析分支河道砂体沉积及煤层厚度变化特征,归纳出本区的聚煤规律,对于优化勘查设计,指导资源勘查及在富煤中心区域开展工作有重要指导意义。
Through previous studies on drilling and exploration data,coal-forming environment,and coal seam thickness variation pattern,have considered that the coal resources in the area have been formed in a terrestrial delta plain,and coal deposit is mainly controlled by distributary channel deposits development on delta plain.After studied the distributary channel sand mass sedimentary and coal thickness variation features,have summed up coal accumulation pattern in the area.The study has important guiding significance in exploration design optimization,coal resources exploration guidance in coal enrichment center area.
作者
白阳
Bai Yang(China Coal Geology Group Co.Ltd.,Beijing 100040)
出处
《中国煤炭地质》
2018年第12期1-4,共4页
Coal Geology of China
关键词
陆相三角洲平原
富煤中心
聚煤规律
苏拉特盆地
terrestrial delta plain
coal enrichment center
coal accumulation pattern
Surat Basin