CRUSMID-3D: Crustal Structure and Mineral Deposit Systems

Continental rifting is associated with successive extensional phases, often leading to final continental breakup and initiation of oceanic spreading. Within the context of global plate tectonics, rifting is a fundamental process starting continent dispersal (Wilson, 1966), but instead paleogeographic models or plate reconstructions generally focus on post-breakup times. The main reason is that ocean spreading typically renders well constrained key

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Quantification and Restoration of the Pre‐Drift Extension Across the NE Atlantic Conjugate Margins During the Mid‐Permian‐Early Cenozoic Multi‐Rifting Phases

Abdelmalak

Gac

Inge

et al. 2023

Tectonics

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CRUSMID-3D: Crustal Structure and Mineral Deposit Systems

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References 37 publications

Quantification and Restoration of the Pre‐Drift Extension Across the NE Atlantic Conjugate Margins During the Mid‐Permian‐Early Cenozoic Multi‐Rifting Phases

Quantification and Restoration of the Pre‐Drift Extension Across the NE Atlantic Conjugate Margins During the Mid‐Permian‐Early Cenozoic Multi‐Rifting Phases

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