Mantle Exhumation and Post‐Rift Magmatism at an Oblique Magma‐Poor Continental Margin

Abstract Continental breakup is a fundamental tectonic process, which leads to seafloor spreading and the generation of oceanic crust. However, the current understanding of continental margins, based largely on 2‐D seismic transects, is inadequate to capture the spatial complexity of crustal evoluti...

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Bibliographic Details
Main Authors: Jie Chen, Sylvie Leroy, Louise Watremez, Adam H. Robinson
Format: Article
Language:English
Published: Wiley 2025-04-01
Series:Geophysical Research Letters
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Online Access:https://doi.org/10.1029/2024GL112069
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