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