INTRA-OCEANIC ARCS OF THE PALEO-ASIAN OCEAN

INTRA-OCEANIC ARCS OF THE PALEO-ASIAN OCEAN

Intra-oceanic arcs (IOAs) form at Pacific-type convergent margins, in the upper “stable” plate, when the subducting plate submerges to the depths of melting, i.e., to ca. 50–100 km. A typical IOA system, such as Mariana-Bonin and the Philippines Sea, consists of subduction zone, fore-arc region with...

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Bibliographic Details
Main Authors:	I. Safonova, A. Kotlyarov, S. Krivonogov
Format:	Article
Language:	English
Published:	Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2017-09-01
Series:	Геодинамика и тектонофизика
Online Access:	https://www.gt-crust.ru/jour/article/view/428

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