摘要
七宝山铜多金属矿床位于江西省萍乡市上栗县境内。矿床构造上位于扬子克拉通与华南造山带接合部位—钦杭结合带。矿床的勘查研究工作自上世纪60年代延续至今,取得了许多地质资料并形成了一些理论认识[1-2]。但是,目前对于矿床的矿石矿物成分及其特征工作还不够细致。本次采用手标本鉴定、镜下鉴定及电镜扫描方法详细研究了主要矿石矿物特征,划分了矿石矿物成矿阶段并进一步完善了矿床成因。
Qibao shan copper polymetallic deposit is located in Shangli County of Jiangxi City, Pingxiang province. The ore deposits are located at the junction of the Yangtze Craton and the Southern China orogenic belt,the Hangzhou Hangzhou orogenic belt. Since the 60 s of the last century, the exploration and research of mineral deposits have been carried out, and many geological data have been obtained and some theoretical knowledge has been formed. But at present, the ore mineral composition and characteristics of the deposit is not meticulous enough. By means of hand specimen identification, microscopic identification and scanning electron microscopy,the characteristics of main ore minerals are studied in detail. The mineralization stages of ore minerals are divided, and the genesis of ore deposits is further improved.
出处
《四川有色金属》
2017年第3期28-30,46,共4页
Sichuan Nonferrous Metals
关键词
矽卡岩型
矿石矿物特征
七宝山
skarn type
ore mineral characteristics
Qibaoshan
