在高压下,水可以进入石英,早已为人工实验所证实。而自然界中石英的水化现象,虽有文献提及,但尚缺乏专门的研究。 近年来,笔者研究变质铁矿时,曾注意到在我国许多地区的变质岩中,都不同程度地发育有石英的水化现象。鉴于这一现象对了解变质作用的环境和条件有一定意义,故作一报道,以供进一步研究。 Under high pressure, water can enter the quartz, has long been confirmed by human experiments. However, the hydration phenomenon of quartz in nature, although mentioned in the literature, lacks specialized research. In recent years, when I studied metamorphic iron ore, I have noticed that in many areas of China metamorphic rocks, quartz hydration is developed to varying degrees. In view of this phenomenon to understand the environment and conditions of metamorphism have some significance, so made a report for further study.