Articles | Volume 12, issue 4
https://doi.org/10.5194/se-12-885-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-12-885-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Kinematics and extent of the Piemont–Liguria Basin – implications for subduction processes in the Alps
Eline Le Breton
CORRESPONDING AUTHOR
Department of Earth Sciences, Freie Universität Berlin, Berlin, Germany
Sascha Brune
Geodynamic Modelling Section, German Research Centre for Geosciences, GFZ Potsdam, Potsdam, Germany
Institute of Geosciences, University of Potsdam, Potsdam, Germany
Kamil Ustaszewski
Institute for Geological Sciences, Friedrich-Schiller-Universität Jena, Jena, Germany
Sabin Zahirovic
EarthByte Group, School of Geosciences, The University of Sydney, Sydney, NSW 2006, Australia
Maria Seton
EarthByte Group, School of Geosciences, The University of Sydney, Sydney, NSW 2006, Australia
R. Dietmar Müller
EarthByte Group, School of Geosciences, The University of Sydney, Sydney, NSW 2006, Australia
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63 citations as recorded by crossref.
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59 citations as recorded by crossref.
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4 citations as recorded by crossref.
- The Maira-Sampeyre and Val Grana Allochthons (south Western Alps): review and new data on the tectonometamorphic evolution of the Briançonnais distal margin A. Michard et al. 10.1186/s00015-022-00419-8
- Missing lawsonite and aragonite found: P–T and fluid composition in meta-marls from the Combin Zone (Western Alps) P. Manzotti et al. 10.1007/s00410-021-01818-0
- Serpentinization, Carbonation, and Metasomatism of Ultramafic Sequences in the Northern Apennine Ophiolite (NW Italy) E. Schwarzenbach et al. 10.1029/2020JB020619
- Late Palaeozoic tectonics in Central Mediterranean: a reappraisal G. Molli et al. 10.1186/s00015-020-00375-1
Discussed (final revised paper)
Latest update: 01 Nov 2024
Short summary
The former Piemont–Liguria Ocean, which separated Europe from Africa–Adria in the Jurassic, opened as an arm of the central Atlantic. Using plate reconstructions and geodynamic modeling, we show that the ocean reached only 250 km width between Europe and Adria. Moreover, at least 65 % of the lithosphere subducted into the mantle and/or incorporated into the Alps during convergence in Cretaceous and Cenozoic times comprised highly thinned continental crust, while only 35 % was truly oceanic.
The former Piemont–Liguria Ocean, which separated Europe from Africa–Adria in the Jurassic,...