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Zhurnal Tekhnicheskoi Fiziki, 2011, Volume 81, Issue 9, Pages 147–149 (Mi jtf9247)  
Brief Communications

Model of a magma flow during the Great Tolbachik Fissure Eruption (Kamchatka)

V. K. Balkhanova, Yu. B. Bashkueva, N. S. Zhatnuevb

a Buryat Scientific Centre of Siberian Branch of the Russian Academy of Sciences
b Russian Academy of Sciences Geological Institute of SB RAS
Full-text PDF (100 kB)
Abstract: A model of magma flow-up through a set of fissure channels during the Great Tolbachik Fissure Eruption observed in Kamchatka in 1975 is suggested. The model is based on the assumption that the magmatic liquid flowing through fissure channels in the lithosphere experiences the Brinkman hydrodynamic resistance. Relationships between the depth of a magmatic source, time of magma flow-up to the Earth’s surface, and velocity of the magma flow through fissure channels to the Earth’s surface are derived.
Received: 29.06.2010
Accepted: 29.12.2010
English version:
Technical Physics, 2011, Volume 56, Issue 9, Pages 1366–1368
DOI: https://doi.org/10.1134/S1063784211090052
Bibliographic databases:
Document Type: Article
Language: Russian
Citation: V. K. Balkhanov, Yu. B. Bashkuev, N. S. Zhatnuev, “Model of a magma flow during the Great Tolbachik Fissure Eruption (Kamchatka)”, Zhurnal Tekhnicheskoi Fiziki, 81:9 (2011), 147–149; Tech. Phys., 56:9 (2011), 1366–1368
Citation in format AMSBIB
\Bibitem{BalBasZha11}
\by V.~K.~Balkhanov, Yu.~B.~Bashkuev, N.~S.~Zhatnuev
\paper Model of a magma flow during the Great Tolbachik Fissure Eruption (Kamchatka)
\jour Zhurnal Tekhnicheskoi Fiziki
\yr 2011
\vol 81
\issue 9
\pages 147--149
\mathnet{http://mi.mathnet.ru/jtf9247}
\elib{https://elibrary.ru/item.asp?id=20325242}
\transl
\jour Tech. Phys.
\yr 2011
\vol 56
\issue 9
\pages 1366--1368
\crossref{https://doi.org/10.1134/S1063784211090052}
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