Redox conditions during crystallization of ultramafic and gabbroic rocks of the Yoko–Dovyren massif (Based on the results of measurements of intrinsic oxygen fugacity of olivine)

Author:

Ariskin A. A.,Fomin I. S.,Zharkova E. V.,Kadik A. A.,Nikolaev G. S.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology,Geophysics

Reference46 articles.

1. R. J. Arculus and J. W. Delano, “Intrinsic oxygen fugacity measurements: techniques and results for spinels from upper mantle peridotites and megacryst assemblages,” Geochim. Cosmochim. Acta, 45, 899–913 (1981).

2. R. J. Arculus, J. W. Delano, S. Loureiro, and A. B. Kersting, “Electrochemical measurements bearing on the oxidation state of the Skaergaard Layered Intrusion,” Contrib. Mineral. Petrol. 102, 376–388 (1989).

3. A. A. Ariskin and G. S. Barmina, “COMAGMAT: development of a magma crystallization model and its petrologic applications,” Geochem. Int. 42 (Suppl. 1), S1–S157 (2004).

4. A. A. Ariskin and L. V. Danyushevsky, “The sulfide COMAGMAT: Modeling R-factor and Cu–Ni–PGE tenors in sulfides for multiple-saturated magmas,” in 12 th International Platinum symposium, Yekaterinburg, Russia, (Yekaterinburg, 2014), Vol. 1, pp. 15–16.

5. A. A. Ariskin, E. G. Konnikov, and E. V. Kislov, “Modeling of the equilibrium crystallization of ultramafic rocks with application to the problems of formation of phase layering in the Dovyren Pluton, Northern Baikal Region, Russia,” Geochem. Int. 41 (2), 107–129 (2003).

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