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岩石的熔化实验研究开始于十九世纪末期。当时仅限于在常压高温条件下进行实验。从本世纪三十年代起,开始进行高温高压的实验研究。塔特和鲍温等人对花岗岩体系进行了系统的研究。布朗、皮温斯基、希塔罗夫、温克勒等人对花岗岩和花岗闪长岩做了大量的熔化实验,并发表了不少专著。根据实验资料他们认为,花岗岩的成分、挥发份的含量(CO_2、P_2O_5、HF、HCl、NH_3等)以及所受压力对岩石的熔化温度都有明显影响。 我国在五十年代后期开始对花岗岩类岩石进行系统的熔化实验工作。近年来开展这方面研究的单位日益增多。
The experimental study of melting of rocks began in the late nineteenth century. At that time, it was limited to experiments under atmospheric pressure and high temperature. From the thirties of this century, the experimental study of high temperature and pressure began. Tate and Bowen and others systematically studied the granite system. Brown, Piwinski, Shitarov, Winkler and others have done a lot of melting experiment on granite and granodiorite, and published many monographs. According to the experimental data, they think that the composition of granite, volatile content (CO_2, P_2O_5, HF, HCl, NH_3, etc.) and the pressure on the melting temperature of rock have a significant impact. In the late 1950s, China began systematic melting experiments on granitic rocks. In recent years, the number of units that carry out this research is increasing.