Mapping upper mantle anisotropy beneath SE France by SKS splitting indicates Neogene asthenospheric flow induced by Apenninic slab roll-back and deflected by the deep Alpine roots-Reference-Cited by-同舟云学术

Mapping upper mantle anisotropy beneath SE France by SKS splitting indicates Neogene asthenospheric flow induced by Apenninic slab roll-back and deflected by the deep Alpine roots

Published:2004-12 Issue:1-2 Volume:394 Page:125-138
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Barruol Guilhem,Deschamps Anne,Coutant Olivier

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference47 articles.

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2. Seismic anisotropy of the French Massif Central and predisposition of Cenozoic rifting and volcanism by Variscan suture hidden in the mantle lithosphere;Babuska;Tectonics,2002

3. A Tertiary asthenospheric flow beneath the southern French Massif Central related to the west Mediterranean extension evidenced by upper mantle seismic anisotropy;Barruol;Earth Planet. Sci. Lett.,2002

4. A quantitative evaluation of the contribution of crustal rocks to the shear wave splitting of teleseismic SKS waves;Barruol;Phys. Earth Planet. Inter.,1993

5. Anisotropy beneath the Pyrenees range from teleseismic shear wave splitting;Barruol;Geophys. Res. Lett.,1995

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