Bakening Volcano. Bibliography
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Дитмар К.В. Поездки и пребывание в Камчатке в 1851–1855 гг. Ч. 1. Исторический отчет по путевым дневникам. СПб.: Имп. Академия наук. 1901. 756 с.
Иванов Б.В. Андезиты Камчатки (справочник химических анализов вулканитов и основных породообразующих минералов) / Отв. ред. Колосков А.В. М.: Наука. 2008. 364 с.
   Annotation
This book is the first work that provides the ultimate data about chemical composition of the Kamchatka Quaternary andesites. Besides the book provides data about a phase analysis of andesites, geochemical composition, REE composition and isotopic analysis of strontium, neodymium and oxygen. The analyses are prominent for their stratification and accurate geological positioning. This allows understanding how the geological events alternated. The paper is focused on the petrogenetic peculiarities of tholeiitic (the 1st type of mantle genesis) and calc-alkali (the 2nd type of mantle-crust genesis) andesites. The book stresses that petrochemical, petrological and isotopic-geochemical correlators play a great role in distinguishing of those two types of andesites. On the basis of petrochemical database we distinguished three trends of the volcanites differentiation: stable, unstable and intermediate. These trends are supposed to be used for the determination of the volcanic activity character and types of the volcanic eruptions.
This book will be helpful as a reference guide to volcanologists, petrographers, geochemists and geologists, to those who study the genesis of volcanic rocks.
Колосков А.В. Изотопно-геохимическая неоднородность плиоцен-четвертичных вулканитов Камчатки и проблема астеносферного диапиризма // Вестник КРАУНЦ. Серия: Науки о Земле. 2020. Вып. 47. № 3. С. 25-57. doi: 10.31431/1816-5524-2020-47-3-25-57.
   Annotation
Isotope-geochemical material for Pliocene-Quaternary volcanoes of the Kamchatka region is generalized on a cartographic basis. The Sr-isotope anomalies of moderate and elevated radiogenicity, geochemically confirmed, are spatially conjugated. This made it possible to interpret these anomalies not only as a reflection of mantle plume material in the composition of volcanic rocks, but also of its hybrid environment, as a consequence of plum-lithosphere remobilization. The presence of multi-directional geochemical trends made it possible to propose the concept of moving boundary values for the composition of indicator rocks of the intraplate type and adakites, which significantly expanded the possibilities of their diagnostics. The isotope-geochemical heterogeneity of basaltoids of the region is generally determined by the peculiarities of concentration of rocks with intraplate and adakite geochemical characteristics, which allows considering the asthenospheric diapirism as the main factor of petrogenesis of Pliocene-Quaternary volcanism in Kamchatka.
Леонов В.Л., Рогозин А.Н., Биндеман И.Н., Бергаль-Кувикас О.В., Кляпицкий Е.С. Выделение новой кальдеры на Камчатке: границы, возраст, комплекс внутрикальдерных отложений, нерешенные вопросы // Вулканизм и связанные с ним процессы. Материалы региональной научной конференции, посвящённой Дню вулканолога. Петропавловск-Камчатский, 30 марта - 1 апреля 2011 г. Петропавловск-Камчатский: ИВиС ДВО РАН. 2011. С. 53-56.
Мелекесцев И.В., Дирксен О.В., Гирина О.А. Гигантский эксплозивно-обвальный цирк и обломочная лавина на вулкане Бакенинг (Камчатка, Россия) // Вулканология и сейсмология. 1998. № 3. С. 12-24.
   Annotation
This study revealed that the giant cirque of Bakening Volcano had been produced by its eruption ca. 8000-8500 carbon-14 year ago. The eruption is supposed to have been heralded by a large earthquake (M > 7) resulting in the collapse and slide of the SE sector of the cone. The landslide unroofed the hydrothermal system and triggered an explosion which was followed by an ash-and-block pyroclastic flow. A rockslide avalanche rolled down into the valley of the Srednyaya Avacha River and travelled as far as 10-11 km along it. The avalanche deposited its debris material over an area of 18-20 km2 measuring 0.4-0.5 km3 in volume. These deposits dammed the river, produced two lakes (Bezymyannoe and Verkhneavacha), and gave birth to a large lahar which traveled along the valley much farther.
Набоко С.И. Современные вулканы и газо-гидротермальная деятельность / Геология СССР. М.: Недра. 1964. Т. 31. С. 303-372.
Новейший и современный вулканизм на территории России / Отв. ред. Лаверов Н.П. М.: Наука. 2005. 604 с.
   Annotation
The actual collective monograph presents the results of both theoretical and experimental studies of the multi-disciplinary problem on volcanic hazard assessment and development of techniques for prediction of catastophic eruptions. The volcanism of Kamchatka and other regions of Russia has been analyzed. On the basis of geological, volcanological and tephrachronological studies including radiocarbon dating, there have been defined certain groups of volcanoes on different stages of evolution. At the same time the problem of determination of the internal structure of volcanic dome using modem theoretical methods and technologies is well investigated. The new techniques of estimation of volcanic hazard were developed. Whenever ti is required, theoretical approaches are confirmed by results of in-field observations.

The book will satisfy the needs of Earth sciences specialists from a variety of backgrounds, volcanology, geo-mechanics, ecology, industrial constuction applications and hazard assessment.
Новограбленов П.Т. Каталог вулканов Камчатки // Известия Государственного географического общества. 1932. Т. 64. Вып. 1. С. 88-99.
Пономарева В.В., Чурикова Т.Г., Мелекесцев И.В., Брайцева О.А., Певзнер М.М., Сулержицкий Л.Д. Позднеплейстоцен-голоценовый вулканизм Камчатки / Изменение окружающей среды и климата: природные и связанные с ними техногенные катастрофы. Том II. Новейший вулканизм северной Евразии: закономерности развития, вулканическая опасность, связь с глубинными процессами и изменениями природной среды и климата. М.: ИГЕМ РАН. 2008. С. 19-40.
   Annotation
Изменение окружающей среды и климата: природные и связанные с ними техногенные катастрофы. Том II. Новейший вулканизм северной Евразии: закономерности развития, вулканическая опасность, связь с глубинными процессами и изменениями природной среды и климата. М., Изд-во ИГЕМ; 2008, с. 19-40
Рогозин А.Н., Леонов В.Л., Бергаль-Кувикас О.В. Необычные игнимбриты Верхнеавачинской кальдеры (Камчатка): строение разрезов и петрохимические особенности // Вулканизм и геодинамика. Материалы V Всероссийского симпозиума по вулканологии и сейсмологии. 2011, Екатеринбург: Институт геологии и геохимии. 2011. С. 234-237.