Deep differentiation of alkali ultramafic magmas: Formation of carbonatite melts

Author:

Ryabchikov I. D.,Kogarko L. N.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology,Geophysics

Reference22 articles.

1. G. P. Brey and I. D. Ryabchikov, “Carbon-dioxide in strongly silica undersaturated melts and origin of kimberlite magmas,” Neues Jhrb. Mineral.-Monatsh. 10, 449–463 (1994).

2. P. Cartigny, F. Pineau, C. Aubaud, and M. Javoy, “Towards a consistent mantle carbon flux estimate: Insights from volatile systematics (H2O/Ce, δD, CO2/Nb) in the North Atlantic mantle (14° N and 34° N),” Earth Planet. Sci. Lett. 265, 672–685 (2008).

3. L. S. Egorov, Ijolite–Carbonatite Plutonism: Evidence from the Maimecha–Kotui Complex, Polar Siberia (Nedra, Leningrad, 1991) [in Russian].

4. A. V. Girnis, “Olivine–orthopyroxene–melt equilibrium as a thermobarometer for mantle-derived magmas,” Petrology 11, 115–127 (2003).

5. J. Keller, A. N. Zaitsev, and D. Wiedenmann, “Primary magmas at Oldoinyo Lengai: the role of olivine melilitites,” Lithos 91, 150–172 (2006).

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