AVACHA DEPRESSION, KAMCHATKA: STRUCTURE OF THE BASEMENT

dc.contributor.author	Popruzhenko S.V.
dc.contributor.author	Aprelkov S.E.
dc.date.accessioned	2021-01-01T09:02:50Z
dc.date.available	2021-01-01T09:02:50Z
dc.date.issued	1998
dc.identifier	https://elibrary.ru/item.asp?id=20945990
dc.identifier.citation	Volcanology & Seismology, 1998, , 6, 785-795
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/21992
dc.description.abstract	The structure of the avacha Depression, covered by a thick sequence of volcanic rocks, volcano-sedimentary deposits, and loose Quaternary sediments of varying origins, was reconstructed using the results of a geological survey, geophysical measurements, and drilling data. The depression had a long tectonic history related to a complex combination of linear faults and ring volcano-tectonic faults that obviously controlled the localization of the Avacha-Koryak group of volcanoes. The structure and origin of the Ketka geothermal field, discovered in the SW side of the depression, are discussed.
dc.subject	Quaternary	en
dc.title	AVACHA DEPRESSION, KAMCHATKA: STRUCTURE OF THE BASEMENT
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary	en
dc.subject.age	Кайнозой::Четвертичная	ru

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