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Mantle heterogeneity drives spreading center dynamics at Arctic Mid-Ocean Ridge
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DOI：10.1016/j.epsl.2026.120276.png)
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Abstract
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• Modeling heterogeneous mantle shows variable thermal structure at Arctic ridge. • Mantle viscosity contrasts create a rheological wall shaping isotherm depths. • Multiphysics modeling reproduces Arctic ridge geophysical features.
Keywords:
Mid-ocean ridges
mantle heterogeneity
plate kinematics
ridge migration
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