NEW DATA ON BONINITE MAGMATISM OF EASTERN KAMCHATKA

dc.contributor.authorOsipenko A.B.
dc.date.accessioned2022-01-12T07:50:48Z
dc.date.available2022-01-12T07:50:48Z
dc.date.issued2003
dc.description.abstractThree 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.identifierhttps://www.elibrary.ru/item.asp?id=13425770
dc.identifier.citationDoklady Earth Sciences, 2003, 391, 6, 892-895
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/34231
dc.titleNEW DATA ON BONINITE MAGMATISM OF EASTERN KAMCHATKA
dc.typeСтатья

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