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Records: 1741
Belousov Alexander, Belousova Marina, Krimer D., Costa F., Prambada O., Zaennudin A. Volcaniclastic stratigraphy of Gede Volcano, West Java, Indonesia: How it erupted and when // Journal of Volcanology and Geothermal Research. 2015. Vol. 301. P. 238-252.
Belousov Alexander, Belousova Marina, Voight Barry Multiple edifice failures, debris avalanches and associated eruptions in the Holocene history of Shiveluch volcano, Kamchatka, Russia // Bulletin of Volcanology. 1999. Vol. 61. № 5. P. 324-342. doi:10.1007/s004450050300.
Belousov Alexander, Voight Barry, Belousova Marina Directed blasts and blast-generated pyroclastic density currents: a comparison of the Bezymianny 1956, Mount St Helens 1980, and Soufrière Hills, Montserrat 1997 eruptions and deposits // Bulletin of Volcanology. 2007. Vol. 69. № 7. P. 701-740. doi:10.1007/s00445-006-0109-y.
Belousov Alexander, Voight Barry, Belousova Marina, Petukhin Anatoly Pyroclastic surges and flows from the 8-10 May 1997 explosive eruption of Bezymianny volcano, Kamchatka, Russia // Bulletin of Volcanology. 2002. Vol. 64. № 7. P. 455-471. doi:10.1007/s00445-002-0222-5.
Belousov Alexander, Walter Thomas R., Troll Valentin R. Large-scale failures on domes and stratocones situated on caldera ring faults: sand-box modeling of natural examples from Kamchatka, Russia // Bulletin of Volcanology. 2005. Vol. 67. № 5. P. 457-468. doi:10.1007/s00445-004-0387-1.
Belousova Marina, Belousov Alexander Prehistoric and 1933 debris avalanches and associated eruptions of Harimkotan Volcano (Kurile Islands) // Periodico di Mineralogia. 1995. № LXIV. P. 99-101.
Bergal-Kuvikas Olga, Bindeman Ilya, Skorkina Anna, Khubaeva Olga Origin of monogenetic volcanoes in Malko-Petropavlovsk zone of the transverse dislocation (Kamchatka): geological setting, geophysical parameters and geochemical data // Abstract volume of the 8th International Maar Conference. Petropavlovsk-Kamchatsky: IVS FEB RAS. 2020. P. 37-38.
Bergal-Kuvikas Olga, Nakagawa Mitsuhiro, Kuritani Takeshi, Muravyev Yaroslav, Malik Nataliya, Klimenko Elena, Amma-Miyasaka Mizuho, Matsumoto Akiko, Shimada Shunjiro A petrological and geochemical study on time-series samples from Klyuchevskoy volcano, Kamchatka arc // Contributions to Mineralogy and Petrology. 2017. Vol. 172. № 5. doi:10.1007/s00410-017-1347-z.
Bergal-Kuvikas Olga, Rogozin Aleksei, Kliapitskiy Evgeniy The role of coastal marine environment in formation the Miocene basaltic andesite ignimbrites at Eastern volcanic belt, Kamchatka // Geophysical Research Abstracts, EGU2019-594. 2019. Vol. 21.
Bessonova E.P., Bortnikova S.B., Gora M.P., Manstein Yu.A., Shevko A.Ya., Panin G.L., Manstein A.K. Geochemical and geo-electrical study of mud pools at the Mutnovsky volcano (South Kamchatka, Russia): Behavior of elements, structures of feeding channels and a model of origin // Applied Geochemistry. 2012. Vol. 27. № 9. P. 1829 - 1843. doi: 10.1016/j.apgeochem.2012.02.018.    Annotation
This study presents data on the geochemical composition of boiling mud pools at the Mutnovsky volcano. The physicochemical characteristics of the pools and the concentrations of major, minor and trace elements in pool solutions vary widely. A comparison of the geochemical compositions of host rocks and solutions indicates that leaching from rocks is not the only source of chemicals in thermal solutions. Geophysical studies reveal the inner structure of thermal fields, which reflect the shapes of the underground reservoirs and feed channels. Using geophysical methods (electrical resistivity tomography and frequency domain investigations), it was shown that the vertical structure and complex geochemical zonation of the feed channels leads to a high contrast in the compositions of the mud solutions. These findings answer questions about the origin and composition of surface manifestations. To elucidate the mechanisms of solution formation, an attempt was made to describe the magmatic fluid evolution and the resulting mixing of waters by physical and mathematical models. The model illustrates fluid migration from a magma chamber to the surface. It is shown that the formation of brines corresponding to the mud pool composition is possible during secondary boiling.

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