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文峪金矿床矿物石英红外吸收光谱、热发光、热爆温度等研究表明，含矿与无矿石英上述特征具明显差异：①含矿石英红外吸收光谱Ｈ２Ｏ吸收峰强，光密度Ｄ１＞Ｄ２，Ｄ２／Ｄ１＜１，无矿石英红外吸收光谱Ｈ２Ｏ吸收峰弱，光密度Ｄ１＜Ｄ２，Ｄ２／Ｄ１＞１；②含矿石英热发光强度低，峰强低于１５０ｃｐｓ，总发光强度低于１００００ｃｐｓ；无矿石英热发光强度高，峰强高于１５０ｃｐｓ，总发光强度大于１００００ｃｐｓ；③含矿石英热爆频温度低，一般为１４０～１８０℃；无矿石英热爆频温度高，一般为４２０～４６０℃。为该区金矿脉合矿性评价提供了重要标志。
Quartz infrared absorption spectroscopy, thermoluminescence and thermal explosion temperature of Wenyu gold deposit show that the above characteristics of ore-bearing and ore-free quartz are obviously different: (1) The absorption peak of H2O in ore-bearing quartz is strong, the optical density is D1> D2, D2 / D1 is less than 1, the infrared absorption spectrum of mineral infrared absorption spectrum of H2O is weak, the optical density is D1 1; (2) the ore containing quartz has low luminescence intensity, peak intensity below 150cps and total luminescence intensity below 10000cps ; Ore-free quartz thermal emission intensity is high, the peak intensity is higher than 150cps, the total luminous intensity is greater than 10000cps; ③ ore containing quartz thermal burst frequency is low, generally 140 ~ 180 ℃; ore-free quartz thermal burst frequency is high, usually 420 ~ 460 ℃. It provides an important symbol for the mineral evaluation of gold deposits in the area.