Mantle Deformation Processes During the Rift‐To‐Drift Transition at Magma‐Poor Margins
Abstract The rift‐to‐drift transition at rifted margins is an area of active investigation due to an incomplete understanding of the spatial and temporal evolution of physical and chemical processes at the ocean‐continent transition (OCT). Deep structures that characterize modern OCTs are often diff...
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| Autors principals: | , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Wiley
2023-11-01
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| Col·lecció: | Geochemistry, Geophysics, Geosystems |
| Matèries: | |
| Accés en línia: | https://doi.org/10.1029/2023GC010924 |
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