论文部分内容阅读
矿床的形成过程与特定地质构造背景下地质流体的产生、运移和聚集有着密切的联系。因此,现在许多的专家学者都致力于研究流体与成矿作用之间的关系,这对于找矿有着指导性意义。1流体类型根据不同地质过程中形成的流体溶质类型、温度特点分类:高温硅钾型、中温碳酸盐型、低温硫酸盐型等。根据流体成因划分:岩浆热液、沉积盆地流体、现代大洋海底热液、变质流体、超临界流体。
The formation process of the deposit is closely related to the generation, migration and accumulation of geological fluids under the specific geological structure. Therefore, many experts and scholars now devote themselves to studying the relationship between fluid and metallogenesis, which is instructive for ore prospecting. 1 fluid type According to the formation of different geological processes fluid solute type, temperature characteristics of the classification: high temperature Si-K type, temperature carbonate type, such as low-temperature sulfate type. According to fluid genesis: magmatic hydrothermal fluids, sedimentary basins, modern oceanic seabed hydrothermal fluids, metamorphic fluids and supercritical fluids.