THE OXIDATION-STATE OF THE EARTHS SUB-OCEANIC MANTLE FROM OXYGEN THERMOBAROMETRY OF ABYSSAL SPINEL PERIDOTITES

THE OXIDATION-STATE OF THE EARTHS SUB-OCEANIC MANTLE FROM OXYGEN THERMOBAROMETRY OF ABYSSAL SPINEL PERIDOTITES

THE oxygen fugacity (fO2), or redox state, of the Earth's mantle is an important parameter in the evolution of mantle-derived magmatic rocks. Most estimates of the upper-mantle redox state have been based on samples of the sub-continental mantle and terrestrial lavas, and estimates of fO2 obtai...

Szczegółowa specyfikacja

Opis bibliograficzny
Główni autorzy:	Bryndzia, L, Wood, B, Dick, H
Format:	Journal article
Język:	English
Wydane:	1989

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