Application of IR and Raman spectroscopy for the determination of the role of oxygen fugacity in the formation of N-[ETH]!-[ETH]z-[ETH] molecules and complexes in the iron-bearing silicate melts at high pressures
Large-scale melting of the Earth's early mantle under the effect of global impact processes was accompanied by the generation of volatiles, which concentration was mainly controlled by the interaction of main N, C, O, and H gas-forming elements with silicate and metallic melts at low oxygen fug...
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Published in | Geochemistry international Vol. 54; no. 13; pp. 1175 - 1186 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
01.12.2016
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Subjects | |
Online Access | Get full text |
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