摘要
青龙山地区冶镁白云岩矿层空间分布范围广,厚度稳定,矿石质量优良,属优质冶镁白云岩矿床,具有良好的开发利用潜力。本文通过研究总结近年来青龙山北段杜家圈南,中段石过顶、童家慢坡等地区的冶镁白云岩矿地质勘查成果,对该地区赋存的7层冶镁白云岩矿矿体特征、矿石质量等进行了归纳、分析和研究,并对矿床成因进行了初步探讨。为青龙山其他区域的冶镁白云岩矿找矿、勘查和开发提供参考。
Magnesium-smelting dolomite is one of the dominant mineral resources in Ningxia, it has a wide range of occurrence in Qinglongshan area. This paper summarizes the geological exploration results of magnesium dolomite ore in recent years of Dujiaquan south in the northern section of Qinglongshan Shigouding and Tongjia Manpo in the middle section of this area,the characteristics and of seven layers of magnesium dolomite ore beds in this area are discussed, and we have generalizations,the genesis of the deposit is preliminarily discussed. The magnesium dolomite strata in Qinglongshan area have a large spatial extension scale, stable thickness variation, excellent ore grade, it is a high quality magnesium-smelting dolomite deposit, it has good development and utilization potential.
作者
郭亚龙
曾亚新
王鹏
GUO Ya-long;ZENG Ya-xin;WANG Peng(Ningxia Branch of China National Geological Exploration Center of Building Materials Industry,Yinchuan 750021,China)
出处
《中国非金属矿工业导刊》
2022年第6期16-19,共4页
China Non-Metallic Minerals industry
关键词
冶镁白云岩
矿体特征
宁夏青龙山
magnesium dolomite
orebody characteristics
Qinglongshan
Ningxia
