OCEANIC COMPLEXES IN THE EAST KUMROCH RANGE, KAMCHATKA

dc.contributor.authorTsukanov N.V.
dc.contributor.authorFedorchuk A.V.
dc.date.accessioned2020-10-06T05:07:29Z
dc.date.available2020-10-06T05:07:29Z
dc.date.issued1989
dc.description.abstractIn East Kamchatka, Cretaceous oceanic rocks are known on the Cape Kamchatskiy peninsula and in the melange zones of the East Ranges. The authors' investigations in 1985-1987 revealed oceanic rocks in the eastern part of the Kumroch Range as well. The previously-identified Veltovaya Formation of this region, consisting of basalts and cherty, carbonaceous and clastic rocks, was thought to be a single stratigraphic section dated as Late Cretaceous to Miocene. Two rock complexes of different compositions (cherty-clastic and cherty-basaltic) and exhibiting tectonic relationships can be identified in the Vetlovaya Formation. In the eastern Kumroch Range there are oceanic rocks that constitute tectonic slabs in similar-age rocks of the ocean-side slope of the island arc. This phenomenon is best explained by accretion of oceanic blocks in middle Paleogene time.
dc.identifierhttps://elibrary.ru/item.asp?id=31089084
dc.identifier.citationTransactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 4, 99-103
dc.identifier.issn0891-5571
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/17730
dc.subjectMioceneen
dc.subject.ageКайнозой::Палеогенru
dc.titleOCEANIC COMPLEXES IN THE EAST KUMROCH RANGE, KAMCHATKA
dc.typeСтатья

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