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一、前言 矿物包裹体作为成矿流体的标本,为地质找矿、成矿理论、地球化学研究提供了成矿流体的温度,压力、盐度、密度、气液相成份、Eh、pH值及稳定同位素等方面证据,已经形成了一门新的学科,在地质学各领域中得到普遍的应用和承认。 作为独立的新学科,有许多问题有待深入进行研究,其中最突出的问题就是包裹体测量数据是否反映了成矿流体的真实情况?包裹体形成的三大假说是否成立?这些问题仅仅通过天然矿物包裹体本身研究是无法解决的。为此,我们在已知条件下,用人工合成矿物包裹体的办法,为解决上述问题提供了有效的途径。
I. INTRODUCTION Mineral inclusions, as the samples of ore-forming fluids, provide the temperature, pressure, salinity, density, gas-liquid composition, Eh, pH and the pH of the ore-forming fluid for geological prospecting, metallogenic theory and geochemical research Stable isotopes and other aspects of evidence, has formed a new discipline, in various fields of geology has been widely used and recognized. As an independent new subject, there are many problems to be studied in depth. The most prominent issue is whether the inclusion measurement data reflect the real situation of ore-forming fluids. Whether the three hypotheses of inclusion formation are established? These problems are solved only by natural minerals The study of the inclusion itself can not be solved. To this end, we know that under the conditions of artificial synthetic mineral inclusions approach to solve these problems provide an effective way.