Spatial variations of seismic attenuation and heterogeneity in the Pyrenees: Coda Q and peak delay time analysis-Reference-Cited by-同舟云学术

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Spatial variations of seismic attenuation and heterogeneity in the Pyrenees: Coda Q and peak delay time analysis

Published:2013-11 Issue: Volume:608 Page:428-439
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Calvet Marie,Sylvander Matthieu,Margerin Ludovic,Villaseñor Antonio

Funder

European Regional Development Fund (ERDF/FEDER) – POCTEFA program – (SISPyr project)

Agence Nationale de la Recherche

Consolider-Ingenio 2010 project TOPO-IBERIA

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference73 articles.

1. Origin of coda waves: source attenuation and scattering effects;Aki;J. Geophys. Res.,1975

2. Notes on ground motion parameters for eastern north America: duration and H/V ratio;Atkinson;Bull. Seismol. Soc. Am.,1993

3. The lithosphere–asthenosphere boundary in the western Mediterranean from 3D joint gravity and geoid modeling: tectonic implications;Ayala;Earth Planet. Sci. Lett.,2003

4. Carte géologique des Pyrénées à 1/400000;Baudin,2008

5. Heat flow and regional uplift at the north-eastern border of the Ebro basin, NE Spain;Cabal;Geophys. J. Int.,1995

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