Lithospheric structure of Iberia and Morocco using finite-frequency Rayleigh wave tomography from earthquakes and seismic ambient noise-Reference-Cited by-同舟云学术

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Lithospheric structure of Iberia and Morocco using finite-frequency Rayleigh wave tomography from earthquakes and seismic ambient noise

Published:2017-05 Issue:5 Volume:18 Page:1824-1840
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Palomeras I.¹²^ORCID,Villaseñor A.³^ORCID,Thurner S.¹,Levander A.¹,Gallart J.³^ORCID,Harnafi M.⁴^ORCID

Affiliation:

1. Rice University; Houston Texas USA

2. Department of Geology; University of Salamanca; Salamanca Spain

3. Institute of Earth Sciences Jaume Almera, ICTJA-CSIC; Barcelona Spain

4. Scientific Institute of Rabat, Université Mohammed V-Agdal; Rabat Morocco

Funder

U.S. National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016GC006657/fullpdf

Reference84 articles.

1. Amaru , M. L. 2007

2. The continental lithosphere: Reconciling thermal, seismic, and petrologic data;Artemieva;Lithos,2009

3. Potential field constraints on the deep structure of the Lugo gneiss dome (NW Spain);Ayarza;Tectonophysics,2007

4. Geophysical constraints on the deep structure of a limited ocean-continent subduction zone at the North Iberian Margin;Ayarza;Tectonics,2004

5. Crustal structure under the central High Atlas Mountains (Morocco) from geological and gravity data;Ayarza;Tectonophysics,2005

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