Physicochemical parameters of the melts participating in the formation of chromite ore hosted in the Klyuchevsky ultramafic massif, the Central Urals, Russia

Author:

Simonov V. A.,Ivanov K. S.,Smirnov V. N.,Kovyazin S. V.

Publisher

Pleiades Publishing Ltd

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference26 articles.

1. F. Bea, G. B. Fershtater, P. Montero, et al., “Recycling of Continental Crust into the Mantle As Revealed by Kytlym Dunite Zircons, Ural Mts., Russia,” Terra Nova 3, 407–412 (2003).

2. L. D. Bulykin, K. K. Zoloev, and A. N. Mardiros’yan, “Ore Formation Types of Chromite Deposits and Related Platinum Group Elements,” in Actual Problems of Magmatic Geology, Petrology, and Ore Formation (Uralgeolkom, Yekaterinburg, 1995), pp. 68–78 [in Russian].

3. L. V. Danyushevsky, “The Effect of Small Amounts of H2O on Crystallization of Mid-Ocean Ridge and Back-Arc Basin Magmas,” J. Volcan. Geotherm. Res., 110,(3–4), 407–412 (2001).

4. A. A. Efimov, Yu. L. Ronkin, S. Zindern, et al., “New U-Rb Data on Zircons from Plagiogranite of the Kytlym Massif: Isotopic Ages of Late Events in the History of the Ural Platinum Belt,” Dokl. Akad. Nauk 403(4), 512–516 (2005) [Dokl.Earth Sci. 403A (6), 896–900 (2005)].

5. L. I. Gurskaya, L. V. Smelova, L. R. Kolbantsev, et al., Platinum Group Elements of Chromite-Bearing Massifs of the Polar Urals (VSEGEI, St. Petersburg, 2004) [in Russian].

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