顏色为鑑定金屬礦物頗为重要的特征。在反光顯微鏡下我們可首先根据反射色这一标誌來区别礦石中的各类伴生礦物。此外我們也常借这一个可被熟記的主观标誌來識認好些常見的礦物。可是侭管如此,直到現在研究或鑑定礦石礦物並未充分地利用反射色这一極有價值的物理性質。反射色未被足夠注視的原因是由于礦物的視覚顏色随着光源及伴生礦物环境的不同而有所改变;另一方面是那怕在特定的观察条件下,每一种礦物虽具有独特的反射顏 Color is a very important feature in the identification of metal minerals. Under the reflective microscope, we can first distinguish the associated minerals in the ore based on the sign of the reflective color. In addition, we often use this one can be memorized subjective signs to recognize the more common minerals. However, this is the case, until until now the study or identification of ore minerals has not fully utilized the valuable physical properties of reflective color. Reflected color is not enough attention because the mineral color depends on the light source and accompanying mineral environment changes; the other hand is that even under certain observation conditions, although each mineral has a unique reflection Yan