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随着地球科学的迅速发展,人们从宏观和微观两个方面进行了大胆的探索.从微观来说,近年来人们对矿物包裹体中气一液相及子晶的研究,有力地推动了矿物和岩石成因理论的发展.尤其是在解决一些长期争论的著名矿床(如世界许多地区都有广泛分布的密西西比式大型层状矿体)的成因和成矿规律以及成矿成岩条件方面,已经取得了很大的成就,已经建立了利用气一液的化学成分研究矿床成因的新理论和新方法.这种新的理论和方法,为普查勘探岩浆期后矿床和一些盲矿体,提供了新的找矿途径,同时,它还可以用于环境科学中准确测定工业废气,以改造和保护人类赖以生存的自然环境.
With the rapid development of earth science, people have made a bold exploration both macroscopically and microscopically.In the microcosm, the research on gas-liquid phase and sub-crystal in mineral inclusions in recent years has strongly promoted the development of minerals And the development of the theory of rock genesis, especially in the resolution of the genesis and mineralization of well-known mineralized deposits (such as the widespread, large-scale Mississippi-type stratigraphic orebodies in many parts of the world) and their metallogenetic diagenetic conditions A great achievement has been made and new theories and methods for studying the origin of deposits using the chemical composition of gas-liquid have been established. This new theory and method have provided new clues for the census and exploration of post-magmatic deposits and some blind ore bodies It also can be used in environmental science to accurately measure industrial waste gas so as to rebuild and protect the natural environment on which human beings depend.