摘要
广东翁源红岭钨矿具有石英脉型钨矿和花岗岩型钨矿两种矿床类型。红岭花岗岩型钨矿赋存于本期燕山三期第三、第四阶段中细粒白云母花岗岩中,矿床具有规模大、品位相对低的特点。研究花岗岩型钨矿的矿床地质特征,有利于总结规律指导下一步矿区的找矿工作。
Hongling deposits in Wenyuan conuty have two kinds of deposit including quartz-vein type tungsten deposit and granite type tungsten deposit. Hongling granitoid lithologie deposit occurs in fine-grained muscovite granite of third and fourth stage of Yanshanian period. Mineral deposit has characteristics of large scale and relatively low grade. Study on geological characteristics of granite type tungsten deposit helps to summarize rules to guide the next step prospecting.
出处
《资源环境与工程》
2015年第3期299-302,318,共5页
Resources Environment & Engineering
关键词
花岗岩型钨矿
矿床地质特征
红岭
granite type tungsten deposit
geological characteristics of deposit
Hongling
