富水流体包体可通过下述方法在天然石英中产生。该方法是将石英在实验室造成裂隙,然后在600℃和2千巴、有水存在的热液装置中局部退火。这种人造流体包体的大小、分布和形态明显地与变质地体中石英的流体包体相似。流体包体看来局限于沿先前的裂隙面的阶梯状线理分布。它们的大小与原始裂隙面上阶梯状线理的间隔成正比,而数量与其成反比。细 The water-rich fluid inclusions can be produced in natural quartz by the method described below. The method is to crack the quartz in the laboratory and then locally anneal it in a hydrothermal plant at 600 ° C and 2 kbar, in the presence of water. The size, distribution and morphology of such artificial fluid inclusions are clearly similar to the quartz fluid inclusions in the metamorphic terrain. The fluid inclusions appear to be limited to the stepwise linear distribution along the previous fracture plane. Their size is proportional to the spacing of staircase-like lines on the original fracture surface, and the number is inversely proportional to it. fine