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对山门银矿床不同成矿阶段的红外光谱及热发光研究结果表明：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评价的指标。含矿与不含矿的石英热发光峰均为单峰形，但不含矿石英高于含矿石英的热发光温度。
The results of infrared spectroscopy and thermoluminescence at different mineralization stages of the Shanmen silver deposit show that the relative absorbance of H_2O (A_1) and CO_2 (A_2) in the quartz inclusions can be used as an indicator of ore-bearing evaluation. The luminescence peaks of both quartz and non-ore-bearing quartz are unimodal, but non-ore quartz is higher than the luminescence temperature of ore-bearing quartz.