Genesis and mechanisms of formation of rare-metal peralkaline granites of the Khaldzan Buregtey massif, Mongolia: Evidence from melt inclusions

Author:

Andreeva I. A.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology

Reference56 articles.

1. Andreeva, I.A., Kovalenko, V.I., Yarmolyuk, V.V., et al., Immiscibility of silicate and salt (Li,Na,F) melts in comendite at the Zaart Khudag ore occurrence, Central Mongolia: evidence from melt inclusions, Dokl. Earth Sci., 2007, vol. 414, no. 1, pp. 655–660.

2. Andreeva, I.A. and Kovalenko, V.I., Evolution of the trachydacite and pantellerite magmas of the bimodal volcanic association of Dzarta-Khuduk, Central Mongolia: investigation of inclusions in minerals, Petrology, 2011, vol. 19, no. 4, pp. 348–369.

3. Andreeva, O.A., Andreeva, I.A., Yarmolyuk, V.V., and Borisovskiy, S.E., Evolution of melts of the Changbaishan Tianchi Volcano (China–North Korea) as a model of ore–magmatic system formation: data from melt inclusions studies, Dokl. Earth Sci., 2016, vol. 466, no. 1, pp. 82–87.

4. Antipin, V.S., Andreeva, I.A., Kovalenko, V.I., and Kuznetsov, V.A., Geochemical specifics of ongonites in the Ary-Bulak Massif, Eastern Transbaikalia, Petrology, 2009, vol. 17, no. 6, pp. 558–569.

5. Badanina, E.V., Thomas, R., Syritso, L.F., et al., High boron concentration in an Li–F granitic melt, Dokl. Earth Sci., 2003, vol. 390, no. 1, pp. 529–532.

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