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Asymptotic viscoacoustic diffraction tomography of ultrasonic laboratory data: a tool for rock properties analysis ArchiMer
Ribodetti, A; Operto, S; Virieux, J; Lambare, G; Valero, Hp; Gibert, D.
This paper presents an application of 2.5-D asymptotic viscoacoustic diffraction tomography to ultrasonic data recorded during a physically scaled laboratory experiment. This scaled experiment was used to test the reliability of our method when applied to a real data set to estimate the attenuation factor Q. Diffraction tomography relies on ray theory to compute the Green functions in a smooth background medium and on the Born approximation to linearize the relation between the scattered wavefield and the velocity and Q perturbations. The perturbations are inferred from the data by an iterative (linear) quasi-Newtonian algorithm. The inversion formula was specifically developed to account for the acquisition geometry designed in this study. The derivation...
Tipo: Text Palavras-chave: Asymptotic method; Attenuation; Diffraction tomography; Rock properties; Ultrasonic seismic data.
Ano: 2000 URL: https://archimer.ifremer.fr/doc/00466/57770/60029.pdf
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Crustal structure deduced from receiver functions via single-scattering migration ArchiMer
Bertrand, E; Deschamps, A; Virieux, J.
An investigation of the teleseismic P -wave coda is performed using the single-scattering approximation. The method allows one to image short-wavelength scale (less than or equal to2 km) velocity and density heterogeneities and structures that are barely detected by traveltime tomography. Source effects are removed by using receiver functions for data interpretation, but the amplitude (especially the sign of the signal) is synthesized. Both broad-band seismological stations in the southwestern Alps (France) and Campanian plain (Italy) are used for the illustration of the proposed method. Because of the large aperture of our arrays, laterally small-scale heterogeneities are difficult to image and we must assume lateral continuity of the detectable...
Tipo: Text Palavras-chave: Body waves; Broad-band; Crustal structure; Moho discontinuity; P-to-S conversions; Scattering; Waveform analysis.
Ano: 2002 URL: https://archimer.ifremer.fr/doc/00466/57762/60036.pdf
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Locating and quantifying the seismic discontinuities in a complex medium through the migration and AVA analysis of reflected and converted waves: an application to the Mt Vesuvius volcano ArchiMer
Auger, E; Virieux, J; Zollo, A.
In this paper, we show how the migration of active seismic data can be used to identify and position a seismic discontinuity in a complex medium, and how the amplitude variations of the converted P to S waves can be interpreted to constrain the seismic velocities below the interface. For the application we turn our attention on Mt Vesuvius, an active volcano threatening a densely populated area. To better define its plumbing system, we investigate a mid-crust seismic discontinuity first identified by Zollo et al. (1996, Science, 274, 592-594) and assumed to be the top of a layer containing low-velocity material. We deduce a reference velocity model from previous works on first arrival times, and use it to migrate PP reflected and PS converted waves. In the...
Tipo: Text Palavras-chave: Crustal structure; Explosion seismology; Low-velocity layer; S waves; Seismic tomography; Volcanic structure.
Ano: 2003 URL: https://archimer.ifremer.fr/doc/00466/57760/60035.pdf
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