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在热液矿物的流体包体中,常常含有子矿物,它们是由被捕获的高温流体冷却时沉淀形成的。通常是据其外表观测特征,如溶解度、磁性、晶形和双折射率等来鉴定它们的。近来采用了更完善的鉴定方法,如单个子矿物的提取和 X 射线衍射分析、喇曼光谱分析以及扫描电镜和定性能散分析的应用等。扫描电镜和定性能散分析(显微探针)可
In the fluid inclusions of hydrothermal minerals, sub-minerals are often contained, which are precipitated as the captured high temperature fluid cools down. Their appearance is usually characterized by their appearance characteristics such as solubility, magnetism, crystal form and birefringence. More sophisticated methods of identification have recently been adopted, such as the extraction of individual daughter minerals and X-ray diffraction analysis, Raman spectroscopy, the use of scanning electron microscopy and the analysis of deterministic energy dispersions. Scanning electron microscopy and qualitative analysis (microprobe) can be