Articles | Volume 12, issue 11
https://doi.org/10.5194/se-12-2633-2021
© 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-12-2633-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Orogenic lithosphere and slabs in the greater Alpine area – interpretations based on teleseismic P-wave tomography
Institut für Geologische Wissenschaften, Freie Universität
Berlin, Malteserstr. 74–100, 12249 Berlin, Germany
Stefan M. Schmid
Institut für Geophysik, ETH-Zürich, Sonneggstr. 5, 8092
Zurich, Switzerland
Marcel Paffrath
Institut für Geologie, Mineralogie, Geophysik,
Ruhr-Universität Bochum, 44780 Bochum, Germany
Wolfgang Friederich
Institut für Geologie, Mineralogie, Geophysik,
Ruhr-Universität Bochum, 44780 Bochum, Germany
For further information regarding the team, please visit the link which appears at the end of the paper.
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- How Alpine seismicity relates to lithospheric strength C. Spooner et al. 10.1007/s00531-022-02174-5
- High-resolution mapping of the mantle transition zone and its interaction with subducted slabs in the Ibero-Maghrebian region J. Parera-Portell et al. 10.1016/j.epsl.2024.118798
- Kinematic reconstruction of the Alpine Tethys and surrounding Mesozoic rifted margins G. Frasca et al. 10.1007/s00531-024-02407-9
- Geophysical‐Petrological Model for Bidirectional Mantle Delamination of the Adria Microplate Beneath the Northern Apennines and Dinarides Orogenic Systems W. Zhang et al. 10.1029/2022JB024800
- Present‐Day Upper‐Mantle Architecture of the Alps: Insights From Data‐Driven Dynamic Modeling A. Kumar et al. 10.1029/2022GL099476
8 citations as recorded by crossref.
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- 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
- Lithosphere Structure, Processes, and Physical State of the Alpine‐Apennine System I. Menichelli et al. 10.1029/2023JB026411
- Miocene high elevation in the Central Alps E. Krsnik et al. 10.5194/se-12-2615-2021
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- Moho and uppermost mantle structure in the Alpine area from S-to-P converted waves R. Kind et al. 10.5194/se-12-2503-2021
- Azimuthal anisotropy from eikonal tomography: example from ambient-noise measurements in the AlpArray network E. Kästle et al. 10.1093/gji/ggab453
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Short summary
New images from the multi-national AlpArray experiment illuminate the Alps from below. They indicate thick European mantle descending beneath the Alps and forming blobs that are mostly detached from the Alps above. In contrast, the Adriatic mantle in the Alps is much thinner. This difference helps explain the rugged mountains and the abundance of subducted and exhumed units at the core of the Alps. The blobs are stretched remnants of old ocean and its margins that reach down to at least 410 km.
New images from the multi-national AlpArray experiment illuminate the Alps from below. They...