Bibliography
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Records: 2772
 M
Mantle and fluid sources below Klyuchevskoy-Kamen-Bezymianny line (Kamchatka) (2014)
Churikova T., Gordeychik B., Wörner G. Mantle and fluid sources below Klyuchevskoy-Kamen-Bezymianny line (Kamchatka) / Geofluid-3. Nature and Dynamics of fluids in Subduction Zones. Tokyo, Japan, February 28 - March 3, 2014. Tokyo, Japan: Tokyo Institute of Technology. 2014. P. 72
   Annotation
Kamen volcano is an extinct volcanic complex located in the central part of the Klyuchevskaya group of volcanoes (KGV) between active Klyuchevskoy, Bezymianny, and Ploskie Sopky volcanoes. Kamen volcano was mapped by V.A. Ermakov only in the 1970s. However the modern geochemical studies of Kamen volcano have not been previously carried out and its relationship and petrogenesis in comparison to other active neighbors are unknown. A modern geochemical study of Kamen volcano is needed because it will shed light not only on the history of the volcano itself and its closest neighbors, but also on the history and magmatic evolution of the KGV melts in general. The distance between the summits of Kamen and Klyuchevskoy is only 5 km, the same as between Kamen and Bezymianny. The close relationship in space and time of the KGV and the common zone of seismicity below them suggests a common source and a possible genetic relationship between their magmas. However, the Late-Pleistocene-Holocene lavas of all these neighboring volcanoes are very different: high-Mg and high-Al Ol-Cpx-Pl basalts and basaltic andesites occur at Klyuchevskoy volcano, and Hbl-bearing andesites and dаcites dominate at Bezymianny volcano. The rocks of Ploskie Sopky volcano, situated only 10 km NW of Kamen, are represented by medium-high-K subalkaline lavas.
Marekanitic-rhyolitic complex of the Okhotsk coast (north-east of the USSR) (1967)
Rudich K.N. Marekanitic-rhyolitic complex of the Okhotsk coast (north-east of the USSR) // Bulletin Volcanologique. 1967. Vol. 30. Vol. 1. P. 123-128. 6 p. doi:10.1007/BF02597662.
Mass balance and thermal regime of a crater glacier at Ushkovskii volcano (1990)
Muravyev Y.D., Salamatin A.N. Mass balance and thermal regime of a crater glacier at Ushkovskii volcano // Volcanology and Seismology. 1990. Vol. 11. № 3. P. 411-424.
   Annotation
Построена теплофизическая модель стационарного состояния ледника в активном кратере Ушковского вулкана. Анализ составляющих баланса массы льда показал повышенный геотермический поток (среднее значение 10 Вт/м¤) в пределах вершинного конуса и слабую его изменчивость за последние 40 лет. По измеренной скорости аккумуляции и распределению температуры в снежнофирновой скорости аккумуляции и распределению температуры в снежно-фирновой толще в центре кратера Горшкова предполагается существование значительного поднятия (вложенного малого кратера), перекрытого ледником.
Полученные расчетные формулы помогут оценить параметры критических состояний нестационарных ледяных масс на склонах Ключевского вулкана.
Mechanical properties of lava extruded in the 1983 Predskazanny eruption (Klyuchevskoi volcano) (1988)
Panov V.K., Slezin Yu.B., Storcheus A.V. Mechanical properties of lava extruded in the 1983 Predskazanny eruption (Klyuchevskoi volcano) // Volcanology and Seismology. 1988. Vol. 7. P. 25-37.
Mechanism of magma ascent and deep feeding channels of island arc volcanoes (1975)
Fedotov S.A. Mechanism of magma ascent and deep feeding channels of island arc volcanoes // Bulletin Volcanologique. 1975. Vol. 39. Vol. 2. P. 241-254. doi: 10.1007/BF02597830.
   Annotation
The paper discusses the mechanism of deep magma activity beneath island are volcanoes and similar structures on the basis of data from geophysical investigations in Kamchatka; the analyses of forces that cause the ascent of magma; and related phenomena that are due to hydrostatic forces.
It is shown that the ascent of magma through the astnenosphere occurs most likely in magma columns with a diameter of approximately 700–2,000 m and with a velocity of about 0.8–3 m/year. A regular line of such columns spaced in Kamchatka at a distance of about 30 km gives rise to a chain of separate Etrge volcanoes or volcanic centers.
Ultrabasic magmas are most likely accumulated near the M discontinuity, whereas the apparent place of andesitic magma accumulation is in the earth’s crust near the boundary between the basement and sediments.
Mechanism of the historical and the ongoing Vulcanian eruptions of Ebeko volcano, Northern Kuriles (2021)
Belousov Alexander, Belousova Marina, Auer Andreas, Walter Thomas R., Kotenko Tatiana Mechanism of the historical and the ongoing Vulcanian eruptions of Ebeko volcano, Northern Kuriles // Bulletin of Volcanology. 2021. Vol. 83. № 4. P. 1-24. doi: 10.1007/s00445-020-01426-z.
Mechanism of volcanic earthquakes of the Sheveluch volcano, Kamchatka (1971)
Zobin V.M. Mechanism of volcanic earthquakes of the Sheveluch volcano, Kamchatka // Bulletin Volcanologique. 1971. Vol. 35. Vol. 1. P. 225-229. 5 p. doi:10.1007/BF02596819.
Melted xenoliths of intrusive rocks in the pyroclastic deposits of the Uzon and Semyatchinskaya ring structures (Kamchatka) (1972)
Bogoyavlenskaya G.E. Melted xenoliths of intrusive rocks in the pyroclastic deposits of the Uzon and Semyatchinskaya ring structures (Kamchatka) // Bulletin Volcanologique. 1972. Vol. 36. Vol. 3. P. 443-445. 3 p. doi:10.1007/BF02597119.
Mercury (Hg) in the near-ground atmosphere of active volcanic edifices in Kamchatka (2008)
Ozerova N., Ozerov A. Mercury (Hg) in the near-ground atmosphere of active volcanic edifices in Kamchatka // 33rd International Geological Congress. Oslo, Norway. Abstracts. 2008.
Mercury in vapor-gas fumarole jets and products of their sedimentation at the Mutnovsky volcano (2011)
Ozerova N.A., Ozerov A.Yu. Mercury in vapor-gas fumarole jets and products of their sedimentation at the Mutnovsky volcano // Commission on the chemistry of volcanic gases (CCVG) - IAVCEI. 11th Gas Workshop, Kamchatka, Russia. 1-10 September 2011. 2011. P. 36