Zobrazeno 1 - 7
of 7
pro vyhledávání: '"S. B. Samoilenko"'
Autor:
T. M. Manevich, S. B. Samoilenko
Publikováno v:
Лëд и снег, Vol 56, Iss 3, Pp 399-412 (2016)
The study of moraines at the Avacha volcano group revealed that glaciers changes at all volcanoes within the group happened almost synchronously. Glacial deposits could be grouped into three generations, corresponding to three periods of glacier fluc
Externí odkaz:
https://doaj.org/article/1b20591efe1d4e5e854d56cddd99decc
Autor:
T. M. Manevich, S. B. Samoilenko
Publikováno v:
Лëд и снег, Vol 52, Iss 3, Pp 25-30 (2015)
The paper presents main glaciological characteristics of present-day glaciers located on the Koryaksky volcano. The results of fieldwork (2008–2009) and high-resolution satellite image analysis let us to specify and complete information on modern g
Externí odkaz:
https://doaj.org/article/4760e0c8dec04653936ef3d9317e65f5
Publikováno v:
Лëд и снег, Vol 55, Iss 3, Pp 14-26 (2015)
The present-day glaciation of the Avachinskaya volcano group was analyzed using data obtained during field works of 2007–2010. Twenty seven glaciers were found on the volcanic slopes with their total area of 24.04±3.6 km2. These glaciers belong to
Externí odkaz:
https://doaj.org/article/dda2250acc7e4db89f7aa42e30a92658
Autor:
A. A. Plechova, S. B. Samoilenko, Maxim Portnyagin, Natalia Gorbach, T. M. Manevich, T. M. Philosofova
Publikováno v:
Journal of Volcanology and Seismology. 12:155-171
This paper presents the results from a study of ash compositions that were erupted in 2013–2016. The juvenile component has been identified in the ejecta using data on the morphology and textural features of ash particles and the composition of vol
Autor:
Evgenii Gordeev, Ya. D. Murav’ev, Dmitry Melnikov, V. N. Dvigalo, A. O. Volynets, S. B. Samoilenko
Publikováno v:
Doklady Earth Sciences. 452:1046-1050
Autor:
Evgenii Gordeev, S. B. Samoilenko
Publikováno v:
Doklady Earth Sciences. 436:275-278
The dynamics of magmatic melts in the near-surface part of several kilometers depth is determined by gas release processes. Formation of free gas share is an energy source, while decreasing of the density of the melt creates conditions for magma moti
Publikováno v:
Heat Transfer Research. 35:207-218