THE STRUCTURAL EVOLUTION OF OCEANIC CORE COMPLEXES: A CONCEPT BASED ON ANALOG MODELING

Oceanic core complexes are lithological assemblages of predominantly peridotites and serpentinites, located along intersections of some slow-spreading oceanic accreting rifts and fracture zones, embedded in the predominantly basaltic oceanic lithosphere, and fresh and old basalts are juxtaposed acro...

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Bibliographic Details
Main Author: Y. Mart
Format: Article
Language:English
Published: Institute of the Earth's crust, Siberian Branch of RAS 2020-03-01
Series:Geodinamika i Tektonofizika
Subjects:
Online Access:https://www.gt-crust.ru/jour/article/view/980