Gravity anomalies, flexure and the thermo-mechanical evolution of the West Iberia Margin and its conjugate of Newfoundland
<p>The West Iberia (WIM) and Newfoundland (NFM) continental margins formed over a succession of rift events related to the opening of the North Atlantic between the Late Triassic and the Early Cretaceous. They are characterized by a variable width Ocean- Continent Transition (Zone) where exhu...
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| Format: | Thesis |
| Language: | English |
| Published: |
2008
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| Subjects: |