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近年来,作者对一些不同类型岩浆岩(花岗岩、霞石正长岩、流纹岩、凝灰熔岩、玄武岩等)矿物中包裹体进行了研究,总结出鉴定熔融(固化)包裹体的特征,并利用南京大学仪器厂生产的LGHS-1型高温加热台对一些岩浆岩进行了成岩温度测定。加热台测温范围0—1450℃±,20℃加热腔体积为0.8立方厘米,温差20—50℃。利用岩石熔融包裹体均匀化温度,可以作为探讨岩浆岩矿物形成温度的一个手段。近十年来,国外在成岩温度测定方面进行了不少工作,对自然界各类岩石的温度进行了较系统的研究,从而丰富了我们对自然地质体形成及其演化规律内在联系的认识,并为深部地质研究提供了宝
In recent years, the authors have studied the inclusions of some different types of magmatic rocks (granite, nepheline syenite, rhyolite, tuff lavas, basalt, etc.), concluded the characterization of the melt (solidified) The diagenesis temperature of some magmatic rocks was determined by using the LGHS-1 high-temperature heating station manufactured by Nanjing University Instrument Factory. Heating station temperature range 0-1450 ℃ ±, 20 ℃ heating chamber volume of 0.8 cubic centimeters, the temperature difference of 20-50 ℃. Using the homogenization temperature of the melt inclusions in rocks can be used as a means to explore the temperature of magmatic rocks. In the last ten years, a lot of work has been done in the determination of diagenetic temperature in foreign countries, and more systematic research has been conducted on the temperature of various types of rocks in the natural world, thus enriching our understanding of the inherent relationship between the formation and evolution of natural geological bodies and Deep geological research provides a treasure