DEPLETED VOLCANISM OF KUNASHIR ISLAND: THE ROLE OF NONSUBDUCTION FACTORS IN THE KURIL ISLAND-ARC MAGMATISM

Martynov Yu.A.; Chashchin A.A.; Martynov A.Yu.; Dril S.I.; Rybin A.V.

dc.contributor.author	Martynov Yu.A.
dc.contributor.author	Chashchin A.A.
dc.contributor.author	Martynov A.Yu.
dc.contributor.author	Dril S.I.
dc.contributor.author	Rybin A.V.
dc.date.accessioned	2022-07-18T05:29:15Z
dc.date.available	2022-07-18T05:29:15Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13451905
dc.identifier.citation	Doklady Earth Sciences, 2004, 394, 1, 124-129
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38244
dc.description.abstract	On the base of geochemical investigation of the main volcanites of Kunashir, Iturup and Paramushir islands (the three largest of the Kuril chain) it was attempted to estimate the respective roles of subduction and nonsubduction factors in petrogenesis of Kuril island arc basalts. Established is the substantial role of nonsubduction factors in magmogenesis of basalts, that is associated with the peculiar geodynamic conditions of Kuril and Japan island-arc systems' junction zone.
dc.title	DEPLETED VOLCANISM OF KUNASHIR ISLAND: THE ROLE OF NONSUBDUCTION FACTORS IN THE KURIL ISLAND-ARC MAGMATISM
dc.type	Статья