NEW DATA ON BONINITE MAGMATISM OF EASTERN KAMCHATKA

dc.contributor.author	Osipenko A.B.
dc.date.accessioned	2022-01-12T07:50:48Z
dc.date.available	2022-01-12T07:50:48Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13425770
dc.identifier.citation	Doklady Earth Sciences, 2003, 391, 6, 892-895
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34231
dc.description.abstract	Three possible scenarios can be proposed for generation of boninite melts in a suprasubduction zone of eastern Kamchatka: (1) plume model [11] that explains specific conditions of boninite petrogenesis under the influence of mantle plume; (2) obduction of lithospheric fragments related to different geodynamic settings (in particular, to spreading in the Komandor Basin of the marginal Bering Sea); and (3) local subduction of a relatively hot microplate.
dc.title	NEW DATA ON BONINITE MAGMATISM OF EASTERN KAMCHATKA
dc.type	Статья

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