Вулкан Синарка. Библиография
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Girina O.A., Loupian E.A., Sorokin A.A., Romanova I.M., Melnikov D.V., Manevich A.G., Nuzhdaev A.A., Bartalev S.A., Kashnitskii A.V., Uvarov I.A., Korolev S.P., Malkovsky S.I., Kramareva L.S. Information Technologies for the Analyzing of Kamchatka and the Kuril Islands Volcanoes Activity in 2019-2020 // Short Paper Proceedings of the VI International Conference on Information Technologies and High-Performance Computing (ITHPC 2021), Khabarovsk, Russia, September 14-16, 2021. Khabarovsk: CEUR-WS.org. 2021. Vol. 2930. P. 112-118.
   Аннотация
The work is devoted to the activity analysis of Kamchatka and the Kuril Islands volcanoes in 2019-2020.The activity of the volcanoes was estimated based on the processing of data from daily satellite monitoring carried out using the information system “Remote monitoring of Kamchatkan and the Kuriles volcanoes activity (VolSatView)”. The activity of the Kamchatka and the Kuril Islands volcanoes considered based on the analysis of their thermal anomalies. Analysis of the characteristics of thermal anomalies over volcanoes was carried out in KVERT IS. Analysis of the temperature of thermal anomalies of volcanoes in the Kuril - Kamchatka region in 2019-2020 shows a significantly higher activity of the Kamchatka volcanoes in comparison with the Kuril volcanoes.
Global Volcanism Program. Volcanoes of the World, v. 4.11.0 (08 Jun 2022). 2013. doi: 10.5479/si.GVP.VOTW4-2013.
   Аннотация
The Volcanoes of the World database is a catalog of Holocene and Pleistocene volcanoes, and eruptions from the past 12,000 years.
Gorshkov G.S. Kurile Islands / Catalog of Active Volcanoes of the World and Solfatara Fields. Rome: IAVCEI, 7. 1958. P. 1-99.
Gorshkov G.S. Volcanism and the Upper Mantle: Investigations in the Kurile Island Arc. New York-London: Plenum Press. 1970. 385 p. doi: 10.1007/978-1-4684-1767-8.
   Аннотация
The present volume seems to me to be a particularly im­ portant one for several reasons. Not least among these is the fact that it summarizes the work of two decades by G. S. Gorshkov, one of the world's leading volcanologists. In addition, it is the first general work of this length on the volcanism of what might be called a "narrow" island arc, a relatively simple megastructure as com­ pared with the "wide" arcs such as Japan and Indonesia. Finally, in this volume Gorshkov has summarized and cited extensive evi­ dence for his general ideas on the relation between volcanism and the earth's crust and mantle. A few potentially troublesome items should be noted here. In the translation the Russian terms "suite" and "series" have been retained, though for American readers these might better have been translated as "formation" and "group. " In almost all cases Russian place names have simply been transliterated rather than translated (e. g. , "Yuzhnyi Isthmus" rather than "South Isthmus"); in a few cases the English equivalent has been given in brackets where this is essential to the understanding of the author's com­ ments. The adjectives have retained their Russian case endings in the process (masculine -yi or -ii, feminine -aya or -'ya, neuter -oe) and this may occasionally lead to some slight confusion, for example, when the author calls a given feature Severnyi Volcano at one point and Severnaya Mountain at another.
Kalacheva Elena, Taran Yuri, Kotenko Tatiana Geochemistry and solute fluxes of volcano-hydrothermal systems of Shiashkotan, Kuril Islands // Journal of Volcanology and Geothermal Research. 2015. Vol. 296. P. 40-54. doi:10.1016/j.jvolgeores.2015.03.010.
   Аннотация
Shiashkotan Island belongs to the Northern Kuril island arc and consists of two joined volcanoes, Sinarka and
Kuntomintar, with about 18 km of distance between the summits. Both volcanoes are active, with historic
eruptions, and both emit fumarolic gases. Sinarka volcano is degassing through the extrusive domewith inaccessible
strong and hot (N400 °C) fumaroles. A large fumarolic field of the Kuntomintar volcano situated in a wide
eroded caldera-like crater hosts many fumarolic vents with temperatures from boiling point to 480 °C. Both
volcanoes are characterized by intense hydrothermal activity discharging acid SO4-Cl waters, which are drained
to the Sea of Okhotsk by streams. At least 4 groups of near-neutral Na-Mg-Ca-Cl-SO4 springs with temperatures in
the range of 50–80 °C are located at the sea level,within tide zones and discharge slightly altered diluted seawater.
Volcanic gas of Kuntomintar as well as all types of hydrothermal manifestations of both volcanoes were collected
and analyzed for major and trace elements and water isotopes. Volcanic gases are typical for arc volcanoes
with 3He/4He corrected for air contamination up to 6.4 Ra (Ra=1.4 ×10−6, the air ratio) and δ13C (CO2) within
−10‰to−8‰VPDB. Using a saturation indices approach it is shown that acid volcanic waters are formed at a
shallow level, whereas waters of the coastal springs are partially equilibrated with rocks at ~180 °C. Trace
element distribution and concentrations and the total REE depend on the water type, acidity and Al+Fe concentration.
The REE pattern for acidic waters is unusual but similar to that found in some acidic crater lake waters.
The total hydrothermal discharge of Cl and S from the island associated with volcanic activity is estimated at
ca. 20 t/d and 40 t/d, respectively, based on the measurements of flow rates of the draining streams and
their chemistry. The chemical erosion of the island by surface and thermal waters is estimated at 27 and 140
ton/km2/year, respectively, which is 2–3 times lower than chemical erosion of tropical volcanic islands.
Siebert L., Simkin T., Kimberly P. Volcanoes of the World. Berkeley: University of California Press. 2010. 568 p.
   Аннотация
This impressive scientific resource presents up-to-date information on ten thousand years of volcanic activity on Earth. In the decade and a half since the previous edition was published new studies have refined assessments of the ages of many volcanoes, and several thousand new eruptions have been documented. This edition updates the book's key components: a directory of volcanoes active during the Holocene; a chronology of eruptions over the past ten thousand years; a gazetteer of volcano names, synonyms, and subsidiary features; an extensive list of references; and an introduction placing these data in context. This edition also includes new photographs, data on the most common rock types forming each volcano, information on population densities near volcanoes, and other features, making it the most comprehensive source available on Earth's dynamic volcanism.
Taran Yuri, Zelenski Mikhail, Chaplygin Ilya, Malik Natalia, Campion Robin, Inguaggiato Salvatore, Pokrovsky Boris, Kalacheva Elena, Melnikov Dmitry, Kazahaya Ryunosuke, Fischer Tobias Gas Emissions From Volcanoes of the Kuril Island Arc (NW Pacific): Geochemistry and Fluxes // Geochemistry, Geophysics, Geosystems. 2018. Vol. 19. Vol. 6. P. 1859-1880. doi: 10.1029/2018GC007477.
   Аннотация
The Kuril Island arc extending for about 1,200 km from Kamchatka Peninsula to Hokkaido Island is a typical active subduction zone with ∼40 historically active subaerial volcanoes, some of which are persistently degassing. Seven Kurilian volcanoes (Ebeko, Sinarka, Kuntomintar, Chirinkotan, Pallas, Berg, and Kudryavy) on six islands (Paramushir, Shiashkotan, Chirinkotan, Ketoy, Urup, and Iturup) emit into the atmosphere > 90% of the total fumarolic gas of the arc. During the field campaigns in 2015–2017 direct sampling of fumaroles, MultiGas measurements of the fumarolic plumes and DOAS remote determinations of the SO2 flux were conducted on these volcanoes. Maximal temperatures of the fumaroles in 2015–2016 were 510°C (Ebeko), 440°C (Sinarka), 260°C (Kuntomintar), 720°C (Pallas), and 820°C (Kudryavy). The total SO2 flux (in metric tons per day) from fumarolic fields of the studied volcanoes was measured as ∼1,800 ± 300 t/d, and the CO2 flux is estimated as 1,250 ± 400 t/d. Geochemical characteristics of the sampled gases include δD and δ18O of fumarolic condensates, δ13C of CO2, δ34S of the total sulfur, ratios 3He/4He and 40Ar/36Ar, concentrations of the major gas species, and trace elements in the volcanic gas condensates. The mole ratios C/S are generally <1. All volcanoes of the arc, except the southernmost Mendeleev and Golovnin volcanoes on Kunashir Island, emit gases with 3He/4He values of >7RA (where RA is the atmospheric 3He/4He). The highest 3He/4He ratios of 8.3RA were measured in fumaroles of the Pallas volcano (Ketoy Island) in the middle of the arc.
Апродов В.А. Вулканы. М.: Мысль. 1982. 367 с.
   Аннотация
Справочник содержит характеристику около трех тысяч вулканов земного шара, сгруппированных по вулканическим поясам и другим районам проявления вулканизма. Этим поясам и районам предшествует их общая геолого-географическая характеристика. Сведения о вулканах включают географическое положение, морфологию, геологическую структуру, активность и т.д. Книга рассчитана не только на специалистов, но и на более широкий круг читателей.
Влодавец В.И. Вулканы Советского Союза / Отв. ред. Головко И.Г. М.: Гос. изд-во географической литературы. 1949. 164 с.
   Аннотация
Среди разнообразных явлений природы вулканическая деятельность во все времена особо привлекала внимание человека. Мощные, величественные, порой мрачные, иногда грозные, но всегда прекрасные, а в древности мало или совсем непонятные картины вулканических извержений производили на людей всегда сильное впечатление. И неудивительно поэтому, что деятельность вулканов вызывала в человеке, с одной стороны, безотчетную тревогу, а с другой — поэтическое восхищение.
Люди различно воспринимают деятельность вулканов. Одни видят в них величественные и грозные явления природы, другие интересуются ими с точки зрения внешней красоты проявления внутренних сил земли, третьих поражает мощь вулканических сил, а четвертые стремятся разобраться во всех вулканических явлениях и выявить причины их— познать их.
Горшков Г.С. Вулканизм Курильской островной дуги / Отв. ред. Рудич К.Н. М.: Наука. 1967. 288 с.
   Аннотация
Работа состоит из двух частей. В первой из них приводятся подробные данные о всех голоценовых вулканах и большинстве плейстоценовых вулканических массивов. Для каждого вулкана приведены данные о форме, строении, петрографии и истории развития. Отдельная глава посвящена петрографическим и петрохимическим особенностям курильских лав. Все вулканологические данные увязаны с особенностями строения земной коры и верхней мантии.
В монографии впервые в мировой вулканологической литературе приводятся такие подробные данные по большому кругу вопросов, на столь обширной территории.
Во второй части рассматриваются петрохимические особенности, а также имеющиеся сведения о строении земной коры и верхней мантии в островных и вулканических дугах, внутри океанических и внутриконтиненталъных вулканах Тихоокеанской области. На большом новом материале подтверждаются выводы о мантийном питании вулканов и о существовании двух главных классов пород — океанического и континентального. Дается схема эволюции вулканизма, как отображение эволюции верхней
мантии.
Книга рассчитана на геологов широкого профиля, а также геофизиков и геохимиков.