广东瑶岭钨矿矿化类型多样性及成矿规律研究  

Study on variety and rule of mineralization in Yaoling tunsten mine in Guangdong province,south China

作　　者：王燕 陈梦熊[2] 李明高 曾永熊 

机构地区：[1]广东省有色金属地质勘查局,广东广州510080 [2]有色金属矿产地质调查中心,北京100012

出　　处：《矿产与地质》2006年第4期334-339,共6页Mineral Resources and Geology

摘　　要：近年来,广东瑶岭钨矿床在原来中型石英脉型黑钨矿床的基础上,又相继发现了花岗岩岩体带附近的矽卡岩型白钨矿化和深部花岗岩体中的构造蚀变岩型白钨矿化。通过对这新老发现的三种类型钨矿化地质特征及成矿规律的总结和归纳,建立了瑶岭不同类型钨矿化成生关系及成矿模式。研究认为,该模式可能会给整个粤北甚至南岭成矿带的地质找矿带来新的启示。Skarn type scheelite mineralization near granitic rocks and structure- alteration type scheelite mineralization have been found one after another in recent year in Yaogang tungsten deposit of Guangdong based on the already known middle type quartz vein type wolframite deposit. The ore forming models and the forming relationship of various types of tungsten mineralization in Yaogang have been established according to the summary of geological characteristics and ore forming regularities of three kinds of tungsten mineralization found soon or after. It is believed by the study that the models will bring new inspiration to the geological prospecting in north Guangdong, even in whole Nanling ore belt.

关 键 词：钨矿床 成矿规律 矿化类型多样性 构造蚀变型白钨矿 矽卡岩型白钨矿 石英脉型黑钨矿 矿化集中区 

分 类 号：P618.67[天文地球—矿床学]