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岩石学的研究令人信服地揭示了岩石产状、结构与构造的大量成因信息,而包含在化学成份中的更多、更重要的潜在成因信息尚远非披露。这一则因为化学成份属微观成因信息,对其探幽索微远不如产状、结构与构造等宏观成因信息那样直观、易于研究;二则受条件所限,岩浆的形成及其成岩成矿过程的高温高压模拟实验远未达到理想境地;第三,岩浆作用是在广泛的空间,漫长的时间和复杂的物理化学环境中进行的,受
Petrological research has convincingly revealed a great deal of genetic information on rock occurrence, structure and tectonics, and more and more important underlying information contained in chemical composition is far from being disclosed. This is because the chemical composition is a microcosmic genetic information that is far less intuitive and easier to be studied than the macroscopic genetic information such as yield, structure and structure of exploration. Second, due to the limited conditions, the formation of magma and its diagenetic mineralization process Of the high-temperature and high-pressure simulation experiments far from the ideal situation; Third, the magma in a wide range of space, long time and complex physical and chemical environment, by