摘要
塔什干库拉玛水泥用灰岩矿赋存于下石炭统多内昔组,为海相沉积矿床,沿走向延伸稳定,厚度变化小,为优质的水泥生产原料。本文总结了库拉玛矿区水泥用灰岩矿体地质、矿石质量变化、矿床成因等特征,为矿山开发利用提供了地质依据。
The Tashkent Kulama limestone deposit for cement, which is hosted in the Lower Carboniferous Donexie formation,is a marine sedimentary deposit with stable extension along strike and little thickness variation, and is a high-quality raw material for cement production. This paper summarizes the geology, ore quality variation, deposit genesis and other characteristics of the limestone deposit for cement in Kulama, which provides a geological basis for the development and utilization of the enterprise.
作者
韩鹏飞
汪凯
崔拥军
寿立永
牛运玖
杨联涛
张晓龙
HAN Peng-fei;WANG Kai;CUI Yong-jun;SHOU Li-yong;NIU Yun-jiu;YANG Lian-tao;ZHANG Xiao-long(Shaanxi Branch of China National Geological Exploration Center of Building Materials Industry,Xi'an 710003,China;Anhui Conch Cement Co.,Wuhu 241000,China)
出处
《中国非金属矿工业导刊》
2022年第5期22-25,37,共5页
China Non-Metallic Minerals industry
关键词
水泥用灰岩矿
地质特征
成因
乌兹别克斯坦
limestone for cement
geological characteristics
genesis of deposit
Uzbekistan