Вакин Е.А., Сугробов В.М. Основные результаты комплексных исследований и их применение при изучении геотермальных месторождений / Геотермические и геохимические исследования высокотемпературных гидротерм. М.: Наука. 1986. С. 189-201.
Гавриленко Г.М., Бондаренко В.И., Гусева В.И., Сазонов А.П., Сергеев В.А., Мальцева В.И., Фазлуллин С.М. Исследования на вулкане Ушишир (Курильские острова) в августе 1983 г. // Вулканология и сейсмология. 1986. № 1. С. 3-12.
Гирина О.А. Инженерно-геологические особенности шлаков Толбачинского дола и их преобразование в ходе поствулканических процессов // Инженерная геология. 1986. № 1. С. 32-38.
An account is given of magnetostratigraphic studies of Kamchatkan Holocene formations: the cover of soil and pyroclastics and the rocks of the cinder cones from the flank eruptions of Klyuchevskoi Volcano. А study was made of seven sections of the soil and pyroclastics and of samples from 17 cinder cones. А detailed account is given of the data processing procedure. Consideration is given to the reasons for the established incompleteness of the paleomagnetic record in the sections and it is demonstrated that adequately detailed reconstruction of the history of the geomagnetic 1ield is possible only provided that а study is made of а series of рагаllеl sections. The trajесtory of the geomagnetic field vector over the last 4000 years is determined on the basis of the material on radiocarbon datings. Seven cycles of paleosecular variations are distinguished in the age range investigated; each of these cycles has individual features by which they can be recognised and used for stratigraphic correlation. The, features taken were the direction of rotation of the vector, the shape and size of its loops, and the length of the cycles. Correlation of the sections based on paleomagnetic data was found to be in good agreement with the tephrostratigraphic correlation and enabled corrections to be made to the age of some horizons, including the archeological layers of the primitive settlement at Zhupanovo and the cinder cones. The metachronous magnetization present in some tephra layers was found to be an obstacle to any improvement in the accuracy and detail of magnetochronological reconstructions.