Formation of primary kimberlite melts – Constraints from experiments at 6–12 GPa and variable CO2/H2O-Reference-Cited by-同舟云学术

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Formation of primary kimberlite melts – Constraints from experiments at 6–12 GPa and variable CO2/H2O

Published:2011-12 Issue:3-4 Volume:127 Page:401-413
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Girnis A.V.,Bulatov V.K.,Brey G.P.

Funder

Russian Foundation for Basic Research

Russian Academy of Sciences

Deutsche Forschungsgemeinschaft

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference33 articles.

1. Stability of high-density clinoenstatite at upper-mantle pressures;Angel;Nature,1992

2. Geochemistry of South African on- and off-craton, group I and group II kimberlites: petrogenesis and source region evolution;Becker;Journal of Petrology,2006

3. Internally-consistent thermodynamic data for minerals in the system Na2O–K2O–CaO–MgO–FeO–Fe2O3–Al2O3–SiO2–TiO2–H2O–CO2;Berman;Journal of Petrology,1988

4. Carbon dioxide in kimberlitic melts;Brey;Neues Jahrbuch für Mineralogie – Monatshefte,1991

5. Experimental melting of carbonated peridotite at 6–10GPa;Brey;Journal of Petrology,2008

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