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岩体型钨(钼)矿,是近几年来被重新认识的、很有找矿前景的一种矿床类型.它具有埋藏浅、品位低、规模大等特点.矿床产于岩体中或接触带上,矿体为岩体的组成部分.具面型蚀变和矿化(亦有线型蚀变叠加).矿石为浸染或细脉浸染状,多数以白钨矿为主.化探对找这类矿床有显著效果.许多岩体型钨(钼)矿床的发现,化探都起了重要作用. 近几年来在粤北地区我队在地质与化探紧密配合下进行岩体型钨(钼)矿床的普查找矿工作,取得了一定的成果,找到了一些矿床和异常区.
Rock type tungsten (molybdenum) ore, is re-recognized in recent years, a very prospecting prospect of a deposit type. It has a shallow burial, low grade, large scale and so on. Deposits produced in the rock mass or contact Belt, the ore body is part of the rock body with surface alteration and mineralization (also a linear alteration superposition) .The ore is disseminated or veinlet disseminated, most of the scheelite mainly. This kind of deposit has remarkable effect.Many rock type tungsten (molybdenum) deposits have found that geochemical exploration played an important role.In recent years, our team in northern Guangdong in geology and geochemical cooperation with rock mass tungsten ( Molybdenum) prospecting prospecting work, and achieved some results, to find some deposits and anomalous area.