Geochemical specifics of ongonites in the Ary-Bulak Massif, eastern Transbaikalia

Author:

Antipin V. S.,Andreeva I. A.,Kovalenko V. I.,Kuznetsov V. A.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology

Reference22 articles.

1. V. S. Antipin, V. A. Kuznetsov, V. I. Kovalenko, and M. A. Mitichkin, “Geochemical Zonality and Crystallization Conditions of the Elvan—Ary-Bulak Ongonite Massif (Transbaikalia),” in IGCP-420 Continental Growth in the Phanerozoic: Evidence from Central Asia, Fourth Workshop, Changchun, China, 2002, (Changchun, 2002), pp. 10–13.

2. V. S. Antipin, B. A. Gaivoronskii, V. P. Sapozhnikov, and V. A. Pisarskaya, “Ongonites of the Sherlova Gora District, Eastern Transbaikalia,” Dokl. Akad. Nauk SSSR 253(1), 228–232 (1980).

3. V. S. Antipin, E. A. Savina, M. A. Mitichkin, and V. I. Perelyaev, “Rare-Metal Lithium-Fluorine Granites, Ongonites, and Topazites of the Southern Baikal Region,” Petrologiya 7(2), 141–155 (1999) [Petrology 7, 147–160 (1999)].

4. V. S. Antipin, C. Halls, M. A. Mitichkin, et al., “Elvanes of Cornwall, England, and South Siberia: Subvolcanic Analogues of Subalkaline Rare-Metal Granites,” Geol. Geofiz. 43(9), 841–851 (2002).

5. Bor-Ming Jahn, Ramon Capdevila, Dunyi Lui, et al., “Sources of Phanerozoic Granitoids in the Transect Bayanhongor-Ulaan Baatar, Mongolia: Geochemical and Nd Isotopic Evidence, and Implications for Phanerozoic Crustal Growth,” J. Asian Earth Sci. 23, 629–653 (2004).

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