指出驾鹿金矿床发现的４０种含氧金矿物呈不同色调的褐、紫、黑等色，多为不规则粒状微细晶集合体，粒径在０．０１ｍｍ～０．５ｍｍ之间；条痕紫、黑色，半金属光泽，不透明；反射多色性显著；摩氏硬度为２～３。Ｘ射线衍射分析表明，大部分的晶体结构可能是由Ａｕ，Ａｇ，Ｃｕ，Ｆｅ或Ｐｂ等金属互化物组成的假立方晶格与一个由β－ＴｅＯ２（可能包括ＰｂＯ或ＣａＯ）组成的斜方晶格的混晶，但不排除它们是含金氧化物的可能性；还有些可能是玻璃质或纳米级矿物，少部分则呈现了准晶态物质的特征。 It is pointed out that the 40 kinds of gold-bearing gold minerals found in the Chalu gold deposit are brown, purple and black with different color tones, mostly irregular granular micro-crystalline aggregates with particle sizes between 0.01mm and 0.5mm. Violet, black, semi-metallic luster, opaque; significant reflection polychrome; Mohs hardness of 2 ~ 3. X-ray diffraction analysis shows that most of the crystal structure may be pseudocubic lattices composed of intermetallic compounds of Au, Ag, Cu, Fe or Pb and a rhombohedral composed of β-TeO2 (possibly including PbO or CaO) Lattice mixed crystal, but does not rule out the possibility of them is a gold oxide; some may be vitreous or nano-scale minerals, a small part of the characteristics of the quasi- crystalline material.