摘要
乌兹别克斯坦昆古尔套矿区石膏矿分布于泽拉夫尚河流域的山间盆地中,矿床赋存于古近系含石膏、白云岩地层中。本文主要对石膏矿床的区域成矿地质背景、矿区地质特征、矿床地质特征等进行了研究,在此基础上分析了石膏矿成因,对今后在乌兹别克斯坦地区相似地质背景下寻找同类型石膏矿床具有指导意义。
The gypsum deposit in the Kungurtao mining area of Uzbekistan is distributed in the intermountain basin of Zerafshan River, and the deposit is hosted in the Paleogene gypsum-bearing and dolomite strata. This paper mainly studies the metallogenic geological background of the gypsum deposit, the geological characteristics of the mining area, the geological characteristics of the ore deposit, and etc. On this basis, the main ore genesis is analyzed, which has guiding significance for future prospecting for the same type of gypsum deposits in similar geological background in Uzbekistan.
作者
朱灿豪
夏天
许同舟
ZHU Can-hao;XIA Tian;XU Tong-zhou(Hubei Branch of China National Geological Exploration Center of Building Materials Industry,Wuhan 430034,China)
出处
《中国非金属矿工业导刊》
2022年第6期23-25,30,共4页
China Non-Metallic Minerals industry
关键词
撒马尔罕州
石膏矿
地质特征
成因分析
Samarkand
gypsum mine
geological characteristics
ore genesis
