EGU21-15825
https://doi.org/10.5194/egusphere-egu21-15825
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Opening of the north-eastern Atlantic and onshore mountain rise controlled by Fennoscandian deep structure

Anna Makushkina1, Benoit Tauzin1,2, Meghan Miller1, Hrvoje Tkalcic1, and Hans Thybo3,4,5
Anna Makushkina et al.
  • 1Australian National University, Research School of Earth Sciences, Canberra, Australia
  • 2Université de Lyon, UCBL, ENS Lyon, CNRS, Laboratoire de Géologie de Lyon, Terre, Planètes, Environnement, Villeurbanne, France
  • 3Eurasia Institute of Earth Sciences, Istanbul Technical University, Istanbul, Turkey
  • 4School of Earth Sciences, China University of Geosciences, Wuhan, China
  • 5Center for Earth Evolution and Dynamics (CEED), University of Oslo, Oslo, Norway

Large-scale topography is thought to be mainly controlled by active tectonic processes. Fennoscandia is located far from any active tectonic setting and yet includes a mountain range along its passive North Atlantic margin. Models proposed to explain the origin of these enigmatic mountains are based on glacial isostatic adjustments, delamination, long-term isostatic equilibration, and dynamic support from the mantle, yet no consensus has been reached. We show that topography along the continental margin of Fennoscandia may be influenced by its deep structure. Fennoscandia formed by amalgamation of Proterozoic and Archean continental blocks; using both S- and P-receiver functions, we discovered that the Fennoscandian lithosphere still retains the original structural heterogeneity and its western margin is composed of three distinct blocks. The southern and northern blocks have relatively thin crust (~40-45 km), while the central block has thick crust (~60 km) that most likely was formed by crustal stacking during the Proterozoic amalgamation. The boundaries of the blocks continue into the oceanic crust as two major structural zones of the North-East Atlantic, suggesting that the Fennoscandian amalgamation structures determined the geometry of the ocean opening.  We found no evidence for mountain root support or delamination in the areas of high topography that could be related with mountain formation. Instead, our results suggest that both crustal and lithospheric heterogeneity of Fennoscandia along the continental margin might have a control on geodynamic forces that support the rise of Scandinavian mountains. 

How to cite: Makushkina, A., Tauzin, B., Miller, M., Tkalcic, H., and Thybo, H.: Opening of the north-eastern Atlantic and onshore mountain rise controlled by Fennoscandian deep structure, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-15825, https://doi.org/10.5194/egusphere-egu21-15825, 2021.

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