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熔融包裹体的特征及其测温方法的研究
引用本文:单林,张文智.熔融包裹体的特征及其测温方法的研究[J].地质科学,1981,0(2):164-170.
作者姓名:单林  张文智
作者单位:1. 抚州地质学院;2. 甘肃207指挥部
摘    要:作者对岩石中的熔融包裹体及其测温方法进行了实验,在淬火法测温方面取得了新的进展,对熔融包裹体的特征进行了较系统的总结。

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收稿时间:1979-09-22
修稿时间:1979-09-22;

THE CHARACTERISTICS OF THE FUSION-INCLUSIONS AND THE METHOD MEASURING FOR TEMPERATURE
Shan Lin,Zhang Wenzhi.THE CHARACTERISTICS OF THE FUSION-INCLUSIONS AND THE METHOD MEASURING FOR TEMPERATURE[J].Chinese Journal of Geology,1981,0(2):164-170.
Authors:Shan Lin  Zhang Wenzhi
Institution:1. Fuzhou Geological College, Jiangxi Province;2. Laboratory No.207
Abstract:The fusion-inclusions were formed as minerals being locked after catching silicate magma in the process of its crystallization.The fusion-inclusions differ from gas-aqueous inclusions in form,characteristic of gas gubbles and solid products,and the change in the heating and cooling process.The quenching method by quartz-glass tubes was used to determine the formation temperature of granite,,monzonite and rhyolite.The results of determination agree well with that published in earlier literatures: granite,850-900℃;monzonite,1050-1100℃;rhyolite,1200-1250℃.
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