摘要
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。
On the basis of studying infrared spectrometry and thermoluminescence of quartz in different mineralization stage, the relative degree of absorptivity of H2O(A1) and CO2(A2) in quartz enclusion can be used for evaluation criteria of ore potentiality. Ore-bearing and ore-free quartz have single thermoluminescence peak, but the thermoluminescence temperature of ore-free quartz is higher than ore-bearing quartz's.
出处
《地质找矿论丛》
CAS
CSCD
1994年第4期73-78,共6页
Contributions to Geology and Mineral Resources Research
