Bibliography
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The Kamchatkan Volcanic Eruption Response Team (KVERT) (2002)
Kirianov V.Yu., Neal C.A., Gordeev E.I., Miller T.P. The Kamchatkan Volcanic Eruption Response Team (KVERT) // USGS Fact Sheet. 2002. Vol. 064-02.
The Klyuchevskoy Volcano Eruption in 1993 and 1994 and Its Activity During the Last Decade (1995)
Bogoyavlenskaya G.E., Ozerov A.Yu., Khubunaya S.A. The Klyuchevskoy Volcano Eruption in 1993 and 1994 and Its Activity During the Last Decade / IUGG XXI General Assembly, 1995, (Abstract VB11B-03). 1995. P. 410
The Main Eruptions of Volcanoes in Kamchatka and Kurile Islands in the 1980 (1987)
Fedotov S.A., Ivanov B.V. The Main Eruptions of Volcanoes in Kamchatka and Kurile Islands in the 1980 // Comptes rendus of the XIX General Assembly of the I.U.G.G.: Vancouver, August 9-22, 1987. 1987. Vol. 2. P. 422
The March - June 1984 Eruption of Klyuchevskoi and its Present State as Estimated from Original Observations (1988)
Tokarev P.I. The March - June 1984 Eruption of Klyuchevskoi and its Present State as Estimated from Original Observations // Volcanology and Seismology. 1988. Vol. 7. № 1. P. 143-148.
The Movement of Block and Ash Flows in Channels (2000)
Girina O.A., Bursik M.I. The Movement of Block and Ash Flows in Channels // Abstracts. AGU Spring Meeting 2000. Washington D.C.: 2000. № V52B-0.
The Ploskie Sopki volcanic massif: Geology, petrochemistry, mineralogy, and petrogenesis (Klyuchevskoi Volcanic Cluster, Kamchatka) (2017)
Flerov G.B., Churikova T.G., Anan'ev V.V. The Ploskie Sopki volcanic massif: Geology, petrochemistry, mineralogy, and petrogenesis (Klyuchevskoi Volcanic Cluster, Kamchatka) // Journal of Volcanology and Seismology. 2017. Vol. 11. Vol. 4. P. 266-284. doi: 10.1134/S0742046317040030.
   Annotation
This paper is concerned with the geological history and petrology of a major polygenic volcanic edifice dating back to Upper Pleistocene to Holocene time. This long-lived volcanic center is remarkable in that it combines basaltic and trachybasaltic magmas which are found in basaltic andesite and trachybasaltic– trachyandesite series. The inference is that the coexisting parent magmas are genetically independent and are generated at different sources at depth in an upper mantle volume. The associated volcanic rocks have diverse compositions, stemming from a multi-stage spatio–temporal crystallization differentiation of the magmas and mixing of these in intermediate chas.
The Plumbing System at the Initial Period of the Young Cone Formation, Avachinsky Volcano (Kamchatka) (2007)
Maximov A.P., Puzankov M.Yu., Bazanova L.I. The Plumbing System at the Initial Period of the Young Cone Formation, Avachinsky Volcano (Kamchatka) // XXIV IUGG General Assembly. July 2-13, 2007, Perugia, Italy. 2007.
The Problem of Genetic Relations between High-Aluminous and High-Magnesian Basalts of the Klyuchevskoi Volcano, Kamchatka (1996)
Ozerov A.Yu., Ariskin A.A., Barmina G.S. The Problem of Genetic Relations between High-Aluminous and High-Magnesian Basalts of the Klyuchevskoi Volcano, Kamchatka // Transactions (Doklady) of the Russian Academy of Sciences. Earth Science Sections. 1996. Vol. 350. № 7. P. 1127-1130.
The Recent Activity of Sheveluch Volcano (2002)
Girina O.A., Chubarova O.S., Senyukov S.L. The Recent Activity of Sheveluch Volcano // Abstracts. 3rd Biennial Workshop on Subduction Processes emphasizing the Kurile-Kamchatka-Aleutian Arcs (JKASP-3). Fairbanks. June 2002. 2002. P. 121-122.
The Rikord Submarine Volcanic Massif, Kuril Island Arc (2018)
Blokh Yu. I., Bondarenko V. I., Dolgal’ A. S., Novikova P. N., Petrova V. V., Pilipenko O. V., Rashidov V. A., Trusov A. A. The Rikord Submarine Volcanic Massif, Kuril Island Arc // Journal of Volcanology and Seismology. 2018. Vol. 12. № 4. P. 252-267. doi:10.1134/S0742046318040024.
   Annotation
Изучено строение подводного вулканического массива Рикорда, состоящего из четырех сливающихся по основанию вулканических построек, и имеющего, скорее всего, четвертичный возраст. На начальных этапах жизни вулканического массива изливались базальтовые и андезибазальтовые лавы. Высокие значения естественной остаточной намагниченности драгированных пород обусловлены большим содержанием однодоменных и псевдооднодоменных зерен титаномагнетита и магнетита. Установлены направления подводящих каналов и наличие периферических магматических очагов. Построена объемная модель центральной части вулканического массива Рикорда, в которой выделено десять крупных магнитовозмущающих блоков, которые, вероятнее всего, являются застывшими субвертикальными подводящими каналами.