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赣南钨矿产于燕山早期黑云母花岗岩体内外接触带,主要属气成—高温热液成因,为含钨石英大脉型及细脉带型矿床。前人对本区主要工业矿物黑钨矿和白钨矿进行过大量的工作,但红外光谱的研究较少。本文仅对上述矿物的红外光谱特征及其影响因素作初步探讨。
The tungsten deposits in southern Jiangxi Province originated both in and outside the contact zone of the early biotite granites in Yanshan area. They are mainly gas-hypero-hydrothermal origin and tungsten-bearing quartz veins and vein-type deposits. The predecessors have done a lot of work on the main industrial minerals wolframite and scheelite in this area, but there are few studies on the infrared spectroscopy. This article only on the infrared spectral characteristics of the minerals and their influencing factors for preliminary discussion.