Chrysocolla & Cobaltoan Calcite 5 wholesale 该矿物形成经历了多期热液成矿作用与后期氧化作用:成矿热液首先析出立方体萤石晶体;随后含汞热液在萤石表面沉积形成辰砂薄膜。经过风化氧化,辉锑矿转变为黄色氧化物,同时部分萤石表面形成晕彩锖层。这种稀有矿物组合兼具很高的观赏价值与地质研究意义。
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