Mesoproterozoic olivine gabbronorites of the Bashkirian anticlinorium, the South Urals: Parental melts and specifics of magma evolution

Author:

Nosova A. A.,Sazonova L. V.,Gorozhanin V. M.,Kuz’menkova O. F.,Dubinina E. O.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology

Reference85 articles.

1. A. A. Alekseev, Riphean-Vendian Magmatism of the Western Slope of the South Urals (Nauka, Moscow, 1984) [in Russian].

2. A. A. Alekseev and G. V. Alekseeva, “Riphean Layered Diabase-Picrite Intrusions of the Southern Cis-Urals,” in Ezhegodnik-1996 (Inst. Geol. Ufimsk. Nauchn. Ts., Ufa, 1998), pp. 149–156 [in Russian].

3. A. A. Alekseev, G. V. Alekseeva, and S. G. Kovalev, Differentiated Intrusion of the Eastern Slope of the Urals (Gilem, Ufa, 2003) [in Russian].

4. S. Arai, “Characterization of Spinel Peridotites by Olivine-Spinel Compositional Relationships: Review and Interpretation,” Chem. Geol. 113, 191–204 (1994).

5. A. A. Ariskin and G. S. Barmina, Simulation of Phase Equilibria during Crystallization of Basaltic Magmas (Nauka, Moscow, 2000) [in Russian].

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