农安—德惠一带松花江西岸陶粒页岩矿床特征及开发前景  

Characteristics and development prospects of ceramic shale deposit along the Songhua River west Bank,Nong'an-Dehui area

作　　者：徐传波[1] 孙立伟[1] 张天翼[1] 屈大鹏[1] 

机构地区：[1]吉林省勘查地球物理研究院,吉林长春130021

出　　处：《吉林地质》2010年第4期66-69,共4页Jilin Geology

摘　　要：吉林省陶粒页岩的开发已有十余年的历史,主要矿石自然类型为白垩系下统嫩江组、青山口组泥岩、粉砂质泥岩,目前已开发利用的矿床主要分布于农安—德惠一带松花江西岸的切割台地,均以零星开采为主,矿石质量各有差异,本文通过对这一带典型矿床地质特征进行对比研究,展望该区陶粒页岩矿开发前景。The ceramic shale has been developed in Jilin Province more than ten years.There are mainly Nenjiang Formation of the lower Cretaceous,mudstone,silty mudstone off Qingshankou Formation in ore types.The deposits are mainly distributed in the Songhua River west Bank,Nongan-Dehui areas.There are many scattered mining areas,showing obvious difference in quality.Through the study off deposit features,proposed the development prospects of the ceramic shale in the study area.

关 键 词：粒页岩矿 矿床地质特征 矿石矿物成分 矿石化学成分 陶粒页岩开发前景 

分 类 号：P612.227[天文地球—矿床学]