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流体包裹体在地质作用中出现是普遍的,它担任着元素迁移的载体、化学反应的活化剂的角色。研究包裹体热力学方法主要是均一法、爆裂法和冷冻法,在地质过程中流体提供着重要的研究信息,包裹体被继续生长的主矿物所封闭,基本不受围岩物质的干扰,保留了当时古流体成分和形成环境。因此,流体包裹体在目前地球科学研究中是重要的依据,广泛应用于矿床学、构造地质学、岩石学、石油勘探、地球内部的流体迁移以及岩浆岩系统的演化过程等地学领域,为解决一些地质问题提供可靠资料。
Fluid inclusions are common in geological processes, acting as a carrier of elemental transport and as a chemical activator. The thermodynamic methods of studying inclusions are mainly the homogenization method, the burst method and the freezing method. The fluid provides important research information in the geological process. The inclusions are closed by the main minerals that continue to grow and are basically free from the interference of the surrounding rock materials. The ancient fluid composition and the formation of the environment. Therefore, fluid inclusions are an important basis in the current geoscience research and are widely used in geology, mineralogy, tectonics, petrology, petroleum exploration, intra-Earth fluid migration and magmatic rock system evolution. Some geological issues provide reliable information.