Melting and subsolidus phase relations in peridotite and eclogite systems with reduced COH fluid at 3–16 GPa-Reference-Cited by-同舟云学术

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Melting and subsolidus phase relations in peridotite and eclogite systems with reduced COH fluid at 3–16 GPa

Published:2014-04 Issue: Volume:391 Page:87-99
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Litasov Konstantin D.,Shatskiy Anton,Ohtani Eiji

Funder

Ministry of Education and Science of Russia

Russian Foundation for Basic Research

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference89 articles.

1. Speculations on the nature and cause of mantle heterogeneity;Anderson;Tectonophysics,2006

2. Pressure and temperature dependence of H solubility in forsterite: An implication to water activity in the Earth interior;Bali;Earth Planet. Sci. Lett.,2008

3. The generation of oxidized CO2-bearing basaltic melts from reduced CH4-bearing upper mantle sources;Ballhaus;Geochim. Cosmochim. Acta,1994

4. Techniques for the control of water fugacity and oxygen fugacity for the experimentation in solid media high-pressure apparatus;Boettcher;J. Geophys. Res.,1973

5. Water in the Earth's mantle;Bolfan-Casanova;Mineral. Mag.,2005

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