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The Bezymyannyi, Shiveluch, and St. Helens volcanoes: A comparative revision of their catastrophic eruptions during the 20th century (2015)
Slezin Yu.B. The Bezymyannyi, Shiveluch, and St. Helens volcanoes: A comparative revision of their catastrophic eruptions during the 20th century // Journal of Volcanology and Seismology. 2015. V. 9. № 5. P. 289-294. doi:10.1134/S0742046315050073.
The Catastrophic Paleolahars of the Elbrus Volcano, Northern Caucasus (1998)
Bogatikov O.A., Melekestsev I.V., Gurbanov A.G., Katov D.M., Puriga A.I. The Catastrophic Paleolahars of the Elbrus Volcano, Northern Caucasus // Doklady Earth Sciences. 1998. V. 362. № 7. P. 951-954.
The Composition of Volcanic Ash and the Dynamics of the 2013–2016 Zhupanovsky Volcano Eruption (2018)
Gorbach N.V., Plechova A.A., Manevich T.M, Portnyagin M.V., Philosofova T.M, Samoilenko S.B. The Composition of Volcanic Ash and the Dynamics of the 2013–2016 Zhupanovsky Volcano Eruption // Journal of Volcanology and Seismology. 2018. V. 12. № 3. P. 155-171. doi: DOI: 10.1134/S0742046318030028.    Annotation
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 volcanic glasses. The data set suggests that the activity of the volcano was phreatomagmatic.
The Elbrus caldera in the northern Caucasus (1998)
Bogatikov O.A., Melekestsev I.V., Gurbanov A.G., Katov D.M., Puriga A.I. The Elbrus caldera in the northern Caucasus // Doklady Earth Sciences. 1998. V. 363 A. № 9. P. 1202-1204.
The Eruption of Bezymianny Volcano on August 7, 2001 (2002)
Girina O.A., Ozerov A.Yu., Nuzhdina I.N., Zelenski M.E. The Eruption of Bezymianny Volcano on August 7, 2001 // Abstracts. 3rd Biennial Workshop on Subduction Processes emphasizing the Kurile-Kamchatka-Aleutian Arcs (JKASP-3). Fairbanks. June 2002. 2002. P. 110-111.
The Eruptions of the Northern Group of Volcanoes on Kamchatka in 1988-1989: Seismological and Geodesic Data (1993)
Zharinov N.A., Gorelchik V.I., Zhdanova E.Yu., Andreev V.N., Belousov A.B., Belousova M.G., Gavrilenko V.A., Garbuzova V.T., Demyanchuk Yu.V., Khanzutin V.P. The Eruptions of the Northern Group of Volcanoes on Kamchatka in 1988-1989: Seismological and Geodesic Data // Volcanology and Seismology. 1993. V. 13. V. 6. P. 649-681.
The Evolutionary Stages and Petrology of the Kekuknai Volcanic Massif Reflecting the Magmatism in the Backarc Zone of the Kuril-Kamchatka Island Arc System. Part II. Petrologic and Mineralogical Features, Petrogenesis Model (2013)
Koloskov A.V., Flerov G.B., Perepelov A.B., Melekestsev I.V., Puzankov M.Yu., Filosofova T.M. The Evolutionary Stages and Petrology of the Kekuknai Volcanic Massif Reflecting the Magmatism in the Backarc Zone of the Kuril-Kamchatka Island Arc System. Part II. Petrologic and Mineralogical Features, Petrogenesis Model // Journal of Volcanology and Seismology. 2013. V. 7. № 2. P. 145-169. doi: 10.1134/S0742046313020048.    Annotation
The Kekuknai massif was formed in the course of tectono-magmatic activity that involved the origin of a shield volcano and a caldera depression with associated emplacement of extrusions that terminated in intense post-caldera areal volcanism. The mineralogical compositions of the massifs rocks have been considered in detail. The use of previously known and newly developed indicator properties of rock-forming minerals allowed the reconstruction of the general picture of the magmatic melt evolution and conditions of rock crystallization (various fluid and water saturation levels, as well as the oxidation state of the system). Essentially island-arc or intraplate characteristics of the massif s rock compositions are found at different stages of development of a single fluid-magmatic system. Decompression evolution of the parent deep-seated basanitic magma occurred via occurrence in intermediate magma chambers of daughter magmas of trachybasalt (pre-caldera stage) or hawaiite (areal volcanism) composition. Subsequent emanate-magmatic differentiation of these melts, combined with crystallization differentiation under changing P-T-f0l conditions, resulted in the formation of the entire diversity of the Kekuknai rocks.

Кекукнайский массив сформировался в результате тектоно-магматической деятельности, выразившейся образованием щитообразного вулкана, кальдерной депрессии с сопутствующим внедрением экструзий, и завершившейся интенсивным посткальдерным ареальным вулканизмом. Проведено детальное рассмотрение особенностей минералогического состава пород массива. Использование уже имеющихся и дополнительно выявленных индикаторных возможностей породообразующих минералов позволило восстановить общую картину эволюции магматических расплавов и условия кристаллизации пород (различная флюидонасыщенность-обводненность и окисленность системы). Существенно островодужные или внутриплитные характеристики в составе пород массива проявлены на разных стадиях развития единой флюидно-магматической системы. Декомпрессионная эволюция материнской глубинной базанитовой магмы была реализована появлением в промежуточных очагах дочерних магм трахибазальтового (докальдерный этап развития системы) или гавайитового (ареальный вулканизм) состава. Дальнейшая эманационно-магматическая дифференциация этих расплавов в сочетании с кристаллизационной дифференциации в условиях меняющейся P-T-f02 обстановки и привела к образованию всего многообразия пород Кекукнайского массива.
The First Geological Data on the Chronology of Holocene Eruptive Activity in the Ichinskii Volcano (Sredinnyi Ridge, Kamchatka) (2004)
Pevzner M.M. The First Geological Data on the Chronology of Holocene Eruptive Activity in the Ichinskii Volcano (Sredinnyi Ridge, Kamchatka) // Doklady Earth Sciences. 2004. V. 395A. № 3. P. 335-337.
The Formation of the Chute and the Channel at the Foot of the Andesitic Dome of Bezymianny Volcano (2000)
Girina O.A., Bursik M.I. The Formation of the Chute and the Channel at the Foot of the Andesitic Dome of Bezymianny Volcano // V52B-02. // Abstracts. AGU Spring Meeting 2000. Washington D.C.: 2000.
The Great Tolbachik Fissure Eruption: Geological and Geophysical Data 1975–1976 (1983)
Fedotov S.A., Markhinin Ye.K. The Great Tolbachik Fissure Eruption: Geological and Geophysical Data 1975–1976. 1983. 354 p.    Annotation
In 1975–1976 a remarkable volcanic eruption took place on the Kamchtka peninsula, part of the Soviet Union's arc of active volcanoes. Dr Fedotov and his colleagues studied the largest basaltic eruption in history, one of the most important volcanic events in the twentieth century. During this prolonged eruption they carried out extensive seismological, geophysical, geodetic and geochemical investigations. The results of this detailed and thorough investigation were collected as a series of papers under the editorship of S. A. Fedotov and collected into this volume, which was originally published by Cambridge in 1983. The result is a classic descriptive work of a major volcanic eruption.





 

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