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...
Main Authors: | , , , , , |
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Format: | Article |
Language: | English |
Published: |
Wiley
2021-06-01
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Series: | Geochemistry, Geophysics, Geosystems |
Subjects: | |
Online Access: | https://doi.org/10.1029/2020GC009624 |