A New Technique for Calculating Oxygen Fugacity of a Magma Using Uraninite in Granites  

作　　者：GUO Jian LI Ziying HUANG Zhizhang LI Xiuzhen ZHANG Yuyan FAN Chou 

机构地区：[1]Beijing Research Institute of Uranium Geology,Beijing 100029,China [2]Key Laboratory of Uranium Resource Exploration and Evaluation Technology,Chinese National Nuclear Corporation,Beijing,China [3]South-Central University for Nationalities,Wuhan 430074,Hubei,China

出　　处：《Acta Geologica Sinica(English Edition)》2021年第2期708-709,共2页地质学报（英文版）

基　　金：financially supported by the National Key R&D Program of China(Grant No.2017YFC0602600);Nuclear Power Development(No.HXS1403);Uranium Geology Research Program of China Nuclear Geology(No.201588)。

摘　　要：Objective Oxygen fugacity is an important physicochemical parameter of magmas in addition to temperature,pressure and elemental concentrations,representing a major research topic in natural and experimental petrology.Aside from oxygen probe work,where a direct measurement is made using an oxygen sensor to detect the oxygen content in the fluid and molten metal.

关 键 词：OXYGEN MAGMA representing 

分 类 号：P619.14[天文地球—矿床学]