The Slab Puzzle of the Alpine‐Mediterranean Region: Insights From a New, High‐Resolution, Shear Wave Velocity Model of the Upper Mantle

Author:

El‐Sharkawy Amr12ORCID,Meier Thomas1,Lebedev Sergei3ORCID,Behrmann Jan H.4ORCID,Hamada Mona2,Cristiano Luigia5,Weidle Christian1ORCID,Köhn Daniel1ORCID

Affiliation:

1. Institute of Geosciences Christian‐Albrechts‐Universität Kiel Germany

2. National Research Institute of Astronomy and Geophysics (NRIAG) Helwan, Cairo Egypt

3. School of Cosmic Physics, Geophysics Section Dublin Institute for Advanced Studies Dublin Ireland

4. GEOMAR Helmholtz Centre for Ocean Research Kiel Germany

5. Deutsches GeoForschungsZentrum (GFZ) Potsdam Germany

Funder

German Academic Exchange Service New Delhi

Science Foundation Ireland

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference174 articles.

1. Structure beneath the Alboran from geodynamic flow models and seismic anisotropy

2. Active and remnant subducted slabs beneath Italy: Evidence from seismic tomography and seismicity;Amato A.;Annals of Geophysics,1993

3. über das Bewegungsbild von Faltengebirgen;Ampferer O.;Jahrbuch der Geologischen Reichsanstalt,1906

4. Savani : A variable resolution whole‐mantle model of anisotropic shear velocity variations based on multiple data sets

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