Redox-controlled mechanisms of C and H isotope fractionation between silicate melt and COH fluid in the Earth’s interior

Redox-controlled mechanisms of C and H isotope fractionation between silicate melt and COH fluid in the Earth’s interior

Abstract The behavior of COH fluids, their isotopes (hydrogen and carbon), and their interaction with magmatic liquids are at the core of understanding formation and evolution of the Earth. Experimental data are needed to aid our understanding of how COH volatiles affect rock-forming processes in th...

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Bibliographic Details
Main Author: Bjorn Mysen
Format: Article
Language:English
Published: SpringerOpen 2018-09-01
Series:Progress in Earth and Planetary Science
Subjects:
Fluid
Solubility
Structure
Spectroscopy
Redox
Stable isotopes
Online Access:http://link.springer.com/article/10.1186/s40645-018-0203-8

Internet

http://link.springer.com/article/10.1186/s40645-018-0203-8

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