罕见多矿物晶体共生标本的综合鉴定

    Comprehensive Identification and Analysis of Rare Mineral Crystal Samples

    • 摘要: 随着我国矿物晶体发掘数量日益增多,对这些矿物晶体样本进行资源、种类及溯源等分析研究,对我国矿产开采与开发具有重要的指导意义。结合在贵州黔南发现的矿物晶体样本,采用显微镜、光谱分析仪等测量仪器对矿物晶体的内在结构、种类组成进行分析,进而对矿物晶体的类型、相关序列及种类进行溯源,并对其所在产地进行鉴别。研究结果显示,样本矿物晶体主要为黄铜矿与菱铁矿,晶体中存在铜、铁等主要元素以及锑、砷等少量元素,通过对这些矿物晶体的起源及形成进行溯源,得出晶体所在的环境为地表包含较多热液的地方,这些矿物晶体经过高强度的地壳运动,形成了较为复杂的地质结构,产地溯源对比显示符合样本产地来源。

       

      Abstract: With the increasing number of mineral crystal excavations in our country, the analysis of resources, types and origins of these mineral crystal samples has important guiding significance for the mining and development of minerals in China. Combined with the mineral crystal samples found in Qiannan, Guizhou, the internal sequence and species composition of ore crystals were analyzed by measuring instruments such as microscopes and spectrum analyzers. Then, the types, related sequences and types of mineral crystals were traced, and their origins were identified. The research results show that the sample mineral crystals are mainly chalcopyrite and siderite, and there are major elements such as copper and iron in the crystals, as well as small amounts of elements such as antimony and arsenic. By tracing the origin and formation of these ore crystals, it is concluded that the environment in which the crystals are located is a place containing more hydrothermal fluids on the surface. These mineral crystals have undergone high-intensity crustal movement to form a relatively complex geological structure. The origin traceability comparison shows that it is in line with the origin of the samples.

       

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