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热液上升时,由于与围岩的反应和温度与压力的降低,它们的物理化学性质不可避免地会发生变化。这种变化的自然结果是近矿蚀变岩石中垂直交代分带的发育。含矿交代岩的垂直分带有着重大的科学和实际意义。这种研究将有助于了解热液在空间上和时间上物理化学演化的模式,矿床和矿石出露的侵蚀面标高,及深部隐促矿化的远景。作者在本文中确立了垂直剖面上矿物的规律变化,并试图表明,这种模式受溶液在空间
As hydrothermal fluids rise, their physicochemical properties inevitably change due to the reaction with the surrounding rock and the reduction of temperature and pressure. The natural consequence of this change is the development of vertical metasomatic zonation in near-ore altered rocks. The vertical zoning of ore-bearing rocks has great scientific and practical significance. Such a study will help to understand the patterns of spa- tial and temporal physicochemical evolution of hydrothermal fluids, the elevation of erosion surfaces exposed by deposits and ores, and the prospect of deep mineralization and mineralization. In this paper, the authors establish the regular variation of minerals in the vertical profile and try to show that this mode is influenced by the solution in space