Crustal thickening in an extensial regime: application to the mid-Norwegian Voring margin.
The structure of the mid-Norwegian volcanic Vøring margin at the onset of the Maastrichtian-Paleocene extension phase reflects the cumulative effect of earlier consecutive rifting events. Lateral structural differences present on the margin at that time are a consequence of migration of the location...
| Published in: | Tectonophysics |
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| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
2004
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| Subjects: | |
| Online Access: | https://research.vu.nl/en/publications/73ff6321-1d38-4127-8f05-9b48da939709 https://doi.org/10.1016/j.tecto.2004.07.049 |
| Summary: | The structure of the mid-Norwegian volcanic Vøring margin at the onset of the Maastrichtian-Paleocene extension phase reflects the cumulative effect of earlier consecutive rifting events. Lateral structural differences present on the margin at that time are a consequence of migration of the location of maximum extension in time between Norway and Greenland. The most important imprints (Moho depth, thermal structure) of these events on the lithosphere are incorporated in a numerical simulation of the final extension phase. We focus on a possible mechanism of formation of the Vøring Marginal High and address the relationship between spatial and temporal evolution of crustal thinning and thickening, uplift of the surface and strength of the lithosphere. It is found that the Vøring Basin formed the s trongest part of the margin which explains why the Maastrichtian-Paleocene rift axis was not located here but instead jumped westward with respect to the earlier rift axes locations. The modeling study predicts that local crustal thickening during extension can be expected when large lateral thermal variations are present in the lithosphere at the onset of extension. Negative buoyancy induced by lateral temperature differences increases downwelling adjacent to the rifting zone; convergence of material at the particular part of the margin is mainly taken up by the lower crust. The model shows that during the final phase of extension, the crust in the Vøring Marginal High area was thickened and the surface uplifted. It is likely that this dynamic process and the effects of magmatic intrusions both acted in concert to form the Marginal High. © 2004 Elsevier B.V. All rights reserved. |
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