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赣南钨矿主要属气成一高温热液成因,为含钨石英大脉型及细脉带型矿床,产于燕山早期黑云母花岗岩体内外接触带。前人对本区主要工业矿物黑钨矿和白钨矿已进行过大量而系统的工作。而这些矿物的红外光谱还未见报导,笔者曾对江西漂圹、西华山、荡萍等点钨矿中的黑钨矿、白钨矿等进行过野外观察采样及室内测试研究。现仅将上述矿物的红外光谱特征、谱带归属及影响因素作初步探讨于下。
The tungsten deposits in Gannan mainly belong to the genesis of gas into a high-temperature hydrothermal. It is a tungsten-bearing quartz vein pattern and a vein belt type deposit. It is produced in the contact zone of the early and late Yanshan biotite granites. The predecessors have done a great deal of systematic work on the major industrial minerals wolframite and scheelite in this area. The infrared spectrum of these minerals has not been reported, I had on the wandering in Jiangxi, Xihuashan, swinging and other tungsten ore tungsten scheelite, scheelite field observation and sampling and laboratory testing. Now only the above-mentioned mineral infrared spectral characteristics, the band attribution and influencing factors for preliminary discussion in the next.