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恩格斯曾经指出,“地质学按其性质来说,主要是研究那些不但我们没有经历过,而且任何人都没有经历过的过程。所以要挖掘出最后的、终极的真理就要费很大的力气,而所得是极少的。”尽管早在1858年,索比就曾明确地提出了用于石英和其他一些透明矿物中气(V)—液(L)相包裹体识别和解释的基本准则。也只是近几十年来,在科学技术的迅猛发展及对矿物反应更为详尽的了解基础上,人们才有可能进一步理解气—液相包裹体作为许多岩石形成过程中存在的挥发相可能样品的重要性。
Engels once pointed out: “Geology, by its very nature, is primarily a study of processes not only we have not experienced, but no one has ever experienced, so digging out the final, ultimate truth can be costly Strength, and little is gained. ”" Although Sobie unequivocally proposed the identification and interpretation of gas (V) -liquid (L) phase inclusions in quartz and other transparent minerals as early as 1858 Basic guidelines. It is only in recent decades that based on a more detailed understanding of the rapid development of science and technology and mineral response, it is possible to further understand the potential of gas-liquid inclusions as possible samples of volatile phases present in rock formation importance.