摘要
章广绢云母矿处于扬子陆块西北部,西临郯庐断裂带皖东段,张八岭台隆北段之南缘,总体构造线为北北东向~近南北向。本矿床为沉积变质型矿床,矿体产在青白口系张八岭岩群西冷岩组中段底层中。本文从矿床地质特征等方面展开分析,总结成矿成因及模式,期望对本地区寻找同类型非金属矿床提供借鉴作用。
Zhangguang sericite mine is located in the northwest of the Yangtze block, west of the east Anhui section of the Tanlu fault zone and the southern margin of the northern section of the Zhangbaling uplift stage. The overall tectonic line is NNE-NS. The deposit is sedimentary metamorphic deposits, and the orebodies were found in the bottom of the middle of the Xileng formation of the Zhangbaling rock group in Qingbaikou system. Based on the geological features of the deposit, this paper summarized the metallogenic genesis and model, which can provide some reference for the same type of non metallic ore deposits in this area.
出处
《世界有色金属》
2016年第12期76-77,共2页
World Nonferrous Metals
关键词
绢云母矿
地质特征
沉积变质型
sericite mine
geological feature
sedimentary metamorphic type
