Bibliography
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Records: 2607
 1983
Markhinin E.K. On the State of Kunashir Island Volcanoes (March, 1974 - May, 1982) // Volcanology and Seismology. 1983. № 1. P. 45-52.
Melekestsev I.V. Ages and stages of development of the Kurile - Kamchatka active volcanoes // Arc Volcanism: Physics and Tectonics. Proceedings of a 1981 IAVCEI Symposium, Arc Volcanism, August-September, 1981, Tokyo and Hakone. Tokyo: Terra Scientific Publishing Co. 1983. P. 230-231.
Naboko S.I., Glavatskikh S.F. Posteruptive Hematite Mineralization // Volcanology and Seismology. 1983. № 1. P. 83-96.
Tokarev P.I. Prediction of the Klyuchevskoi Parasitic Eruption in March 1983 // Volcanology and Seismology. 1983. № 5. P. 491-496.
Tokarev P.I. Volcanic Explosions. On the concept of "Volcanic Explosion" // Volcanology and Seismology. 1983. № 3. P. 315-322.
Volynets O.N., Flerov G.B., Andreev V.N., Popolitov E.I., Abramov V.A., Petrov L.L., Shcheka S.A., Selivanova G.I. Geochemical features of the rocks of the Great Tolbachik Fissure Eruption 1975–1976 in relation to petrogenesis / The Great Tolbachik Fissure Eruption. Cambridge: Cambridge University Press. Cambridge: Cambridge University Press. 1983. P. 116-140.
Балуев Э.Ю., Базанова Л.И., Ананьев В.В. Смешение магм по данным изучения вкрапленников плагиоклаза в эффузивных породах Карымского вулканического центра Камчатки // Вулканология и сейсмология. 1983. № 4. С. 41-52.
Бибикова Е.В., Кирнозова Т.И., Максимов А.П., Макаров В.А. Исследование изотопного состава свинца андезитов вулкана Безымянного (Камчатка) // Геохимия. 1983. № 2. С. 163-171.
   Annotation
The results of determination of lead isotope composition in 5 samples of andesites of the Bezymyanny volcano, belonging to the Klyuchevskaya group of volcanoes, are given. Most of the andesites are identical in lead isotopy to basalts of this area and to tholeiites of the ocean ridges. Rocks of the upper mantle or their derivatives could be the source of andesite magmas of volcanoes belonging to the Klyuchevskaya group. At some ca¬ses contamination of andesite magma by the material of upper parts of the crust could occur but it did not play a significant role in the andesite genesis. Facies and mineralogical varieties of the andesites are mainly analogous in lead isotopy so a contamination of rich in water rocks of the crust could not be a cause of appearance of the hornblende andesites.
Брайцева О.А., Егорова И.А., Сулержицкий Л.Д. Тефрохронологические и палинологические исследования в районах активного вулканизма // Известия АН СССР. Серия географическая. 1983. № 6. С. 84-91.
Кирсанов И.Т., Озеров А.Ю. Состав продуктов и энергетический эффект извержения вулкана Горелый в 1980-1981 гг. // Вулканология и сейсмология. 1983. № 1. С. 25-42.