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Чурикова Т.Г., Гордейчик Б.Н., Ивамори Х., Накамура Х., Ишизука О., Нишизава Т., Харагучи С., Миясаки Т., Вагларов Б.С. Геохимическая эволюция Толбачинского массива / Вулканизм, биосфера и экологические проблемы. Восьмая международная научная конференция. Сборник материалов. Туапсе, 1-6 октября 2016 г.. Майкоп-Туапсе: Адыгейский государственный университет. 2016. С. 43-45.
Шанцер А.Е., Цикунов А.Г., Масуренков Ю.П., Ананьев В.В., Балуев Э.Ю. Неогеновая история развития вулканического центра, первый ритм вулканизма / Вулканический центр: строение, динамика, вещество. М.: Наука. 1980. С. 116-125.
Эрлих Э.Н. Гореть - и никаких гвоздей / Вулканы, события, люди. Петропавловск-Камчатский: ИВ ДВО РАН. Петропавловск-Камчатский: ИВ ДВО РАН. 2002. С. 25-28.
Яффе Г.А. Усиление деятельности вулканов Палласа и Сноу / Зап. Приморского филиала Геогр. об-ва СССР.. 1965. Т. 24.
Bergal-Kuvikas Olga Geochemical studies of volcanic rocks from the northern part of Kuril-Kamchatka arc: Tectonic and structural constraints on the origin and evolution of arc magma. 2015. Дисс. канд. геол.-мин. наук.
Riley Colleen Origin of scatter in paleomagnetic directions of samples from Gorely Volcano, Kamchatka, Russia. 1994. Дисс. докт. геол.-мин. наук. 70 p.    Annotation
Lava flows from sixteen sites at Gorely Volcano, Kamchatka were sampled. Initial analysis showed high within-site scatter for NRM specimen directions. Alternating field and thermal demagnetization of specimens showed single-component magnetization indicating that specimens had not moved or were not exposed to changes in the magnetic field during acquisition of a magnetic direction. Scatter is thought to be either due to movement of the specimen with respect to the magnetic field or change in the magnetic field with respect to the specimen. Four factors were found that would contribute to scatter in specimen directions. These are 1) cooling rate, 2) range of unblocking temperatures, 3) relative time of emplacement, and 4) how the specimen moved or was affected by changes in the magnetic field. Only two sites showed that scatter was due to movement of the specimen. It appears that scatter in other sites resulted from changes in the magnetic field generated from a magma-induced electrical current due to lava flowing in the earth’s magnetic field. These changes in the magnetic field are shown to have more affect on material sampled at the surface than on material sampled at depth because massive interiors of flows showed less dispersion in specimen directions than levees or pull-aparts.
Балуев Э.Ю. Петрология Карымского вулканического центра (Восточная Камчатка). 1991. Автореф. дисс. канд. геол.-мин. наук.
Башарина Л.А. Вулканические газы Камчатки. 1966. Автореф. дисс. канд. геол.-мин. наук. 30 с.
Вакин Е.А. Гидрогеология современных вулканических структур и гидротермальные системы Юго-Востока Камчатки. 1968. Автореф. дисс. канд. геол.-мин. наук. 24 с.
Гирина О.А. Современные пирокластические отложения вулканов Камчатки и их инженерно-геологические особенности. 1994. Автореф. дисс. канд. геол.-мин. наук. 23 с.

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