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通过对海沟金矿床石英的红外光谱及热发光研究，获得如下认识：石英包体中Ｈ＿２Ｏ（Ａ＿１）和ＣＯ＿２（Ａ＿２）的相对吸光度可作为含矿性定量的评价指标，即Ａ１＜０．６和Ａ＿２＜０．１２含矿性差；０．６＜Ａ＿１＜ｌ．１和０．１２＜Ａ＿２＜ｌ．３５含矿性比较好Ａ＿１＞ｌ．１和人＞ｌ．３５含矿性好。石英的热发光曲线属双峰型舍矿性好，单峰型含矿性差或不含矿。同时用上述两种方法划分成矿阶段及确定矿体的埋藏深度也具有一定的实际意义。
Through the infrared spectroscopy and thermoluminescence study of the quartz in the Haigou gold deposit, the following understandings are obtained: The relative absorbances of H 2 O (A 1) and CO 2 (A 2) in the quartz inclusions can be used as evaluation indexes of the ore-bearing quantitative index, ie A1 <0.6 And A_2 <0.12 poor oreability; 0.6 l. 1 and person> l. 35 contains good mineral. Quartz’s heat-emitting curve is a bimodal type of homes is good, unimodal with or without mineral deposits. At the same time, it is also of practical significance to classify the ore-forming stage and determine the burial depth of the ore body by using the above two methods.