Impact of sub-basalt thrust systems on the Faroe continental shelf for the late Paleoproterozoic–Cenozoic tectonic evolution of the margin.
The Faroe Island margin is crosscut by late Paleoproterozoic Laxfordian-Nagssugtoqidian thrust systems, which controlled further tectonic development of the margin.
Authors
- David W. Jolley (ORCID: https://orcid.org/0000-0003-0909-2952)
- G. R. Foulger (ORCID: https://orcid.org/0000-0001-6943-6214)
- Alexander L. Peace (ORCID: https://orcid.org/0000-0001-7846-3898)
- Jhon M. Muñoz‐Barrera (ORCID: https://orcid.org/0000-0001-6802-1623)
- Jean-Baptiste P. Koehl (ORCID: https://orcid.org/0000-0001-7189-1988)
Institutions
- Planetary Science Institute (US)
- University of Oslo (NO)
- Durham University (GB)
- University of Aberdeen (GB)
- University of Cundinamarca (CO)
- University of Bergen (NO)
- McGill University (CA)
- McMaster University (CA)
Publication Details
- Journal
- Open Research Europe
- Published
- 2024-08-13
- DOI
- https://doi.org/10.12688/openreseurope.18284.1
- Citations
- 1
- Primary Topic
- Geological Studies and Exploration
- Type
- article
- Field-Weighted Citation Impact
- 0.83
Funders
- Horizon 2020 Framework Programme