Iron carbide as a source of carbon for graphite and diamond formation under lithospheric mantle P-T parameters-Reference-Cited by-同舟云学术

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Iron carbide as a source of carbon for graphite and diamond formation under lithospheric mantle P-T parameters

Published:2017-08 Issue: Volume:286-287 Page:151-161
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Bataleva Yuliya V.,Palyanov Yuri N.,Borzdov Yuri M.,Bayukov Oleg A.,Zdrokov Evgeniy V.

Funder

Russian Foundation for Basic Research

State Assignment

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference57 articles.

1. Volatile-rich metasomatism in Montferrier xenoliths (Southern France): implications for the abundances of chalcophile and highly siderophile elements in the subcontinental mantle;Alard;Journal of Petrology,2011

2. Is the upper mantle metal-saturated?;Ballhaus;Earth and Planetary Science Letters,1995

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

4. Interaction of iron carbide and sulfur under P-T conditions of the lithospheric mantle;Bataleva;Doklady Earth Sciences,2015

5. Conditions for diamond and graphite formation from iron carbide at the P-T parameters of lithospheric mantle;Bataleva;Russian Geology and Geophysics,2016

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