摘要
小龙钨矿床位于泰和县城115°方位,直距约40km处,该矿床发现于1924年,1955年开始机械化开采,迄今已历经58年开采,期间曾开展过多层次多阶段的地质工作。根据小龙钨矿床成矿地质背景,矿区地层、构造、岩浆岩等地质要素,矿体地质特征等方面入手,综合分析了矿区钨矿床主要的成矿控矿因素及矿化富集规律,从而进一步指导地质找矿工作。
Xiaolong wolfram deposit is located 115° direction to Taihe County with a distance about 40kin from county. Xiaolong wolfram deposit, found in 1924, mechanized mined in 1955, has been mining for 58 years, since then multi-level and multi-stage of geological works had been done during those years. According to the mineralizing geological background, stratigraphy, tectonic, magmatic rocks and other geological factors and ore geological characteristics of Xiaolong wolfram deposit area, the mineralize controlling factors and ore enrichment regularity of the mine area are comprehensively analyzed, thereby guide the further geological prospecting work.
出处
《西部探矿工程》
CAS
2014年第5期91-94,96,共5页
West-China Exploration Engineering
关键词
钨矿床
地质特征
富集规律
小龙
wolfram deposit
geological characteristics
enrich-ment regular
Xiaolong
