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...

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Príomhchruthaitheoirí: M. R. Handy, S. M. Schmid, M. Paffrath, W. Friederich
Formáid: Alt
Teanga:English
Foilsithe / Cruthaithe: Copernicus Publications 2021-11-01
Sraith:Solid Earth
Rochtain ar líne:https://se.copernicus.org/articles/12/2633/2021/se-12-2633-2021.pdf