Cenozoic Dynamic Topography of Madagascar

Abstract It has been proposed that Oligo‐Miocene regional uplift of Madagascar was generated and is maintained by mantle dynamical processes. Expressions of regional uplift include flat‐lying Upper Cretaceous‐Paleogene marine limestones that crop out at elevations of hundreds of meters along the wes...

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Bibliographic Details
Main Authors: S. N. Stephenson, N. J. White, A. Carter, D. Seward, P. W. Ball, M. Klöcking
Format: Article
Language:English
Published: Wiley 2021-06-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2020GC009624