Travel time inversion from ground level to gallery: protocol for the characterization of P‐wave seismic signature in a fractured‐porous Urgonian platform at hectometric scale-Reference-Cited by-同舟云学术

Travel time inversion from ground level to gallery: protocol for the characterization of P‐wave seismic signature in a fractured‐porous Urgonian platform at hectometric scale

Published:2014-01 Issue:6 Volume:12 Page:697-708
ISSN:1569-4445
Container-title:Near Surface Geophysics
language:en
Short-container-title:Near Surface Geophysics

Author:

Maufroy Emeline¹²,Gaffet Stéphane¹³,Operto Stéphane¹,Guglielmi Yves⁴,Boyer Daniel³

Affiliation:

1. GEOAZUR, UMR 7329Université de Nice Sophia‐AntipolisCNRSIRDObservatoire de la Côte d’Azur Sophia‐Antipolis Valbonne F‐06560 France

2. Université Grenoble AlpesISTerreUMR 5275CNRSIRDIFSTTAR Grenoble F‐38041 France

3. LSBBUMS 3538Université de Nice Sophia‐AntipolisUniversité d’Avignon et des Pays de VaucluseCNRSAix Marseille UniversitéObservatoire de la Côte d’Azur La grande combe Rustrel F‐84400 France

4. CEREGEUMR 7330Aix Marseille UniversitéCNRSIRD Marseille F‐13331 France

Publisher

Wiley

Subject

Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.3997/1873-0604.2014025

Reference39 articles.

1. Paleogeography of the Urgonian limestones of the Southern France;Arnaud‐Vanneau A.;Geobios,1979

2. Seismic anisotropy analysis at the Low‐Noise Underground Laboratory (LSBB) of Rustrel (France);Bereš J.;Journal of Applied Geophysics,2013

3. Seismic response of a hill: the example of Tarzana, California;Bouchon M.;Bulletin of the Seismological Society of America,1996

4. Seismic imaging of complex onshore structures by 2D elastic frequency‐domain full‐waveform inversion;Brossier R.;Geophysics,2009

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