Elastic versus acoustic 3-D Full Waveform Inversion at the East Pacific Rise 9°50′N

Author:

Marjanović Milena1ORCID,Plessix René-Édouard2,Stopin Alexandre2,Singh Satish C1

Affiliation:

1. Equipe de Geosciences Marines, Institut de Physique du Globe de Paris, 1 rue Jussieu, F-75238 Paris Cedex 05, France

2. Shell Global Solutions International B.V., Grasweg 31, 1031 HW Amsterdam, The Netherlands

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference31 articles.

1. Hydrothermal alteration of a section of upper oceanic crust in the eastern equatorial Pacific: a synthesis of results from Site 504 (DSDP legs 69, 70, and 83, and ODP legs 111, 137, 140, and 148);Alt;Proc. Ocean Drill. Program, Sci. Results,1996

2. Nature of upper crust beneath the Lucky Strike volcano using elastic full waveform inversion of streamer data;Arnulf;Geophys. J. Int.,2014

3. Strong seismic heterogeneity in layer 2A near hydrothermal vents at the mid-Atlantic ridge;Arnulf;Geophys. Res. Lett.,2011

4. The domain of applicability of acoustic full-waveform inversion for marine seismic data;Barnes;Geophysics,2009

5. Evaluation of morphological indicators of magma supply and segmentation from a seismic reflection study of the EPR 15°30′-17° N;Carbotte;J. geophys. Res.,2000

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