滇东黔西上二迭统峨嵋山玄武岩中的煤系及其地层意义  

Upper Permian Amisanseong Basalt Formation of Coal and Its Stratigraphy Signification of East Yunnan and West Quizhou

作　　者：干晓锐 

机构地区：[1]云南能源职业技术学院,曲靖655001

出　　处：《北京工业职业技术学院学报》2007年第3期64-67,共4页Journal of Beijing Polytechnic College

摘　　要：滇东北—黔西南一带的二迭系峨嵋山玄武岩(P2β)中夹有一套厚度不大的陆相含煤岩系,部分地区具有可采煤层,有一定的开发利用价值。简要介绍了此套含煤岩系的分布及特征,并对其地层意义进行简单论述。Among the Permian Amisanseong Basalt （P2β）of Northeast Yunnan-Northwest Guizhou Area, there is a not thick terrigenous Rocks, which contains the formation of coal, partial of which contains mineable coal that has certain development and utilization value. This paper introduces the distribution and characteristic of the rocks, and does a brief appraisement to the significance of the stratum.

关 键 词：玄武岩 煤系 成煤环境 地层划分 

分 类 号：TD163.1[矿业工程—矿山地质测量]