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自第二次世界大战以后带有挥发份的硅酸盐体系的高温高压实验研究得到了飞跃发展,从而代替了战前的以所谓“干燥”体系高温研究为主要阶段的局面。由于高温高压技术的进步,目前已开始对深部地质进行模拟实验研究。美国学者曾做了许多有关地质的高温高压实验研究,而且目前正在大力加强这一工作,前不久美国的马薩诸色工艺研究所的
Since the Second World War with volatile silicate system of high temperature and pressure experimental research has been leapfrog development, which replaced the pre-war so-called “dry” system of high-temperature research as the main stage of the situation. Due to the advancement of high temperature and high pressure technology, simulation experiments on deep geology have been started. American scholars have done a lot of high temperature and pressure on geology experimental research, and is now greatly strengthened this work, not long ago the Massachusetts Institute of Technology in the United States