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The structural evolution of oceanic core complexes: A concept based on analog modeling
Y. Mart
Department of Evolutionary and Environmental Biology
Department of Geography and Environmental Studies
Department of Maritime Civilizations
Research output
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peer-review
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Keyphrases
Analogue Modelling
100%
Asthenosphere
20%
Basalt
40%
Concept Base
100%
Contact Plane
20%
Continent-ocean Boundary
20%
Density Contrast
20%
Density Difference
20%
Diapirism
20%
Fracture Zone
100%
Friction
20%
Friction Constraints
20%
Large Section
20%
Lithological Assemblage
20%
Low Friction
20%
Normal Fault
40%
Oceanic Core Complex
100%
Oceanic Lithosphere
20%
Oceanic Ridge Subduction
20%
Peridotite
60%
Petrology
20%
Rift Zone
20%
Seafloor
20%
Serpentinite
60%
Serpentinization
20%
Slow Spreading
40%
Slow-spreading Ridge
20%
Structural Evolution
100%
Subducting Slab
40%
Subduction
40%
Tectonics
20%
Thermal Gradient
20%
Underthrust
60%
Volcanism
20%
Earth and Planetary Sciences
Asthenosphere
20%
Basalt
40%
Continent
20%
Diapirism
20%
Fracture Zone
100%
Lithosphere
20%
Oceanic Lithosphere
20%
Peridotite
60%
Petrology
20%
Serpentinite
60%
Serpentinization
20%
Structural Evolution
100%
Tectonics
20%
Volcanism
20%