Mechanisms of Partial Melting of Metasomatized Mantle Ultramafic Rocks beneath Avacha Volcano, Kamchatka, and the Growth of Minerals from a Gas Phase in Fractures-Reference-Cited by-同舟云学术

Mechanisms of Partial Melting of Metasomatized Mantle Ultramafic Rocks beneath Avacha Volcano, Kamchatka, and the Growth of Minerals from a Gas Phase in Fractures

Published:2020-11 Issue:6 Volume:28 Page:569-590
ISSN:0869-5911
Container-title:Petrology
language:en
Short-container-title:Petrology

Author:

Sharapov V. N.,Tomilenko A. A.,Kuznetsov G. V.,Perepechko Yu. V.,Sorokin K. E.,Mikheeva A. V.,Semenov Y. I.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology

Link

http://link.springer.com/content/pdf/10.1134/S0869591120050069.pdf

Reference65 articles.

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2. Aharonov, E., Whitehead, J.A., Kelemen, P.B., and Spiegelman, M., Channeling instability of upwelling melt in the mantle, J. Geophys. Res., 1995, vol. 100, pp. 20433–20450.

3. Arai, S. and Ishimaru, S., Insights into petrological characteristics of the lithosphere mantle wedge beneath arcs through peridotite xenoliths: a review, J. Petrol., 2008, vol. 49, no. 4, pp. 359–395.

4. Artem’ev, S.R., Analysis of existing concepts on traditional methods of growth of metallic filiform crystals. Precipitation of matter from gas phase, Tekhnol. Audit Rezerv. Proizvodstva, 2016, vol. 29, no. 3, pp. 34–37.

5. Balashov, V.N. and Likhtner, P.Ch., Disappearing zones in infiltration metasomatic zoning, Dokl. Akad. Nauk SSSR, 1991, vol. 321, pp. 1242–1246.