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PLUTONIC STRUCTURE OF THE DEEP-SEA BASINS IN THE SEA OF OKHOTSK REGION

The original continental crust of the deep-sea basins in the Sea of Okhotsk region was considerably reworked by tectonic and magmatic processes, whereby it has become substantially denser while less thick. The subcrustal lithospheric mantle of the South Okhotsk basin is characterized by the high vel...

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Detalhes bibliográficos
Main Authors: V. P. Semakin, A. V. Kochergin, T. I. Pitina
Formato: Artigo
Idioma:Inglês
Publicado em: Institute of the Earth's crust, Siberian Branch of RAS 2018-03-01
Colecção:Geodinamika i Tektonofizika
Assuntos:
Acesso em linha:https://www.gt-crust.ru/jour/article/view/523
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