跨构造环境的氧逸性

E. Cottrell, S. Birner, M. Brounce, F. Davis, L. Waters, Katherine A. Kelley
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引用次数: 58

摘要

实验和观测证实了氧逸度(fO2)在确定火成岩分异过程中的中心作用,从而为氧气压计的研制和应用提供了理论依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
OXYGEN FUGACITY ACROSS TECTONIC SETTINGS
Experiment and observation have established the centrality of oxygen fugacity (fO2) to determining the course of igneous differentiation, and so the development and application of oxybarometers hav...
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