Abstract
The passive margin of Western Iberia (WIM) developed during the Mesozoic over the pre‐existing Variscan Orogen. In the present study we use integrated interpretation and modelling to understand the distribution of Variscan basement provinces in the offshore of Iberia. The NW‐SE trending fabric of the Variscan Orogen can be recognized in the WIM, and different Variscan basement provinces behaved differently during extension. Furthermore, major Variscan structures reactivated in extension, compartmentalizing rifting and having a major impact on the final architecture of the WIM.
Original language | English |
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Pages (from-to) | 424-432 |
Number of pages | 9 |
Journal | Terra Nova |
Volume | 34 |
Issue number | 5 |
Early online date | 23 Apr 2022 |
DOIs | |
Publication status | Published - Oct 2022 |
Austrian Fields of Science 2012
- 105106 Geodynamics
- 105124 Tectonics
Keywords
- GALICIA CONTINENTAL-MARGIN
- OCEAN
- NEWFOUNDLAND
- EVOLUTION
- INSIGHTS
- GRAVITY