Orogenic lithosphere and slabs in the greater Alpine area – interpretations based on teleseismic P-wave tomography
<p>Based on recent results of AlpArray, we propose a new model of Alpine collision that involves subduction and detachment of thick (<span class="inline-formula">∼</span> 180 km) European lithosphere. Our approach combines teleseismic P-wave tomography and existing local...
Guardado en:
Autores principales: | M. R. Handy, S. M. Schmid, M. Paffrath, W. Friederich |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Copernicus Publications
2021
|
Materias: | |
Acceso en línea: | https://doaj.org/article/53c9102ec2f64b08995bcdba8da97fb8 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Imaging structure and geometry of slabs in the greater Alpine area – a P-wave travel-time tomography using AlpArray Seismic Network data
por: M. Paffrath, et al.
Publicado: (2021) -
Moho and uppermost mantle structure in the Alpine area from S-to-P converted waves
por: R. Kind, et al.
Publicado: (2021) -
U–Pb dating of middle Eocene–Pliocene multiple tectonic pulses in the Alpine foreland
por: L. Smeraglia, et al.
Publicado: (2021) -
Ground-penetrating radar signature of Quaternary faulting: a study from the Mt. Pollino region, southern Apennines, Italy
por: M. Ercoli, et al.
Publicado: (2021) -
Very early identification of a bimodal frictional behavior during the post-seismic phase of the 2015 <i>M</i><sub>w</sub> 8.3 Illapel, Chile, earthquake
por: C. Twardzik, et al.
Publicado: (2021)