TOMO3D: 3-D joint refraction and reflection traveltime tomography parallel code for active-source seismic data-synthetic test

17 pages, 11 figures, 1 table, supporting Information http://gji.oxfordjournals.org/content/203/1/158/suppl/DC1

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Main Authors: Meléndez, Adrià, Korenaga, Jun, Sallarès, Valentí, Miniussi, A., Ranero, César R.
Other Authors: Ministerio de Ciencia e Innovación (España)
Format: artículo biblioteca
Published: Oxford University Press
Subjects:Inverse theory, Controlled source seismology, Seismic tomography,
Online Access:http://hdl.handle.net/10261/124227
http://dx.doi.org/10.13039/501100004837
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spelling dig-icm-es-10261-1242272019-09-26T11:11:54Z TOMO3D: 3-D joint refraction and reflection traveltime tomography parallel code for active-source seismic data-synthetic test Meléndez, Adrià Korenaga, Jun Sallarès, Valentí Miniussi, A. Ranero, César R. Ministerio de Ciencia e Innovación (España) Repsol Inverse theory Controlled source seismology Seismic tomography 17 pages, 11 figures, 1 table, supporting Information http://gji.oxfordjournals.org/content/203/1/158/suppl/DC1 Published by Oxford University Press on behalf of The Royal Astronomical Society. We present a new 3-D traveltime tomography code (TOMO3D) for the modelling of active-source seismic data that uses the arrival times of both refracted and reflected seismic phases to derive the velocity distribution and the geometry of reflecting boundaries in the subsurface. This code is based on its popular 2-D version TOMO2D from which it inherited the methods to solve the forward and inverse problems. The traveltime calculations are done using a hybrid ray-tracing technique combining the graph and bending methods. The LSQR algorithm is used to perform the iterative regularized inversion to improve the initial velocity and depth models. In order to cope with an increased computational demand due to the incorporation of the third dimension, the forward problem solver, which takes most of the run time (~90 per cent in the test presented here), has been parallelized with a combination of multi-processing and message passing interface standards. This parallelization distributes the ray-tracing and traveltime calculations among available computational resources. The code's performance is illustrated with a realistic synthetic example, including a checkerboard anomaly and two reflectors, which simulates the geometry of a subduction zone. The code is designed to invert for a single reflector at a time. A data-driven layer-stripping strategy is proposed for cases involving multiple reflectors, and it is tested for the successive inversion of the two reflectors. Layers are bound by consecutive reflectors, and an initial velocity model for each inversion step incorporates the results from previous steps. This strategy poses simpler inversion problems at each step, allowing the recovery of strong velocity discontinuities that would otherwise be smoothened. © The Authors 2015 AM is funded by Repsol through the CO-DOS collaboration project with CSIC, and the work in this paper was carried at the Grup de Recerca de la Generalitat de Catalunya 2009SGR146: Barcelona Center for Subsurface Imaging (B-CSI) of the Institut de Ciències del Mar (CSIC). Part of this work was also financed by the MICINN project POSEIDON (CMT2010-21569) Peer Reviewed 2015-10 2015-11-02T08:17:47Z artículo http://purl.org/coar/resource_type/c_6501 doi: 10.1093/gji/ggv292 issn: 0956-540X e-issn: 1365-246X Geophysical Journal International 203(1): 158-174 (2015) http://hdl.handle.net/10261/124227 10.1093/gji/ggv292 http://dx.doi.org/10.13039/501100004837 Publisher's version http://dx.doi.org/10.1093/gji/ggv292 No open Oxford University Press
institution ICM ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-icm-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del ICM España
topic Inverse theory
Controlled source seismology
Seismic tomography
Inverse theory
Controlled source seismology
Seismic tomography
spellingShingle Inverse theory
Controlled source seismology
Seismic tomography
Inverse theory
Controlled source seismology
Seismic tomography
Meléndez, Adrià
Korenaga, Jun
Sallarès, Valentí
Miniussi, A.
Ranero, César R.
TOMO3D: 3-D joint refraction and reflection traveltime tomography parallel code for active-source seismic data-synthetic test
description 17 pages, 11 figures, 1 table, supporting Information http://gji.oxfordjournals.org/content/203/1/158/suppl/DC1
author2 Ministerio de Ciencia e Innovación (España)
author_facet Ministerio de Ciencia e Innovación (España)
Meléndez, Adrià
Korenaga, Jun
Sallarès, Valentí
Miniussi, A.
Ranero, César R.
format artículo
topic_facet Inverse theory
Controlled source seismology
Seismic tomography
author Meléndez, Adrià
Korenaga, Jun
Sallarès, Valentí
Miniussi, A.
Ranero, César R.
author_sort Meléndez, Adrià
title TOMO3D: 3-D joint refraction and reflection traveltime tomography parallel code for active-source seismic data-synthetic test
title_short TOMO3D: 3-D joint refraction and reflection traveltime tomography parallel code for active-source seismic data-synthetic test
title_full TOMO3D: 3-D joint refraction and reflection traveltime tomography parallel code for active-source seismic data-synthetic test
title_fullStr TOMO3D: 3-D joint refraction and reflection traveltime tomography parallel code for active-source seismic data-synthetic test
title_full_unstemmed TOMO3D: 3-D joint refraction and reflection traveltime tomography parallel code for active-source seismic data-synthetic test
title_sort tomo3d: 3-d joint refraction and reflection traveltime tomography parallel code for active-source seismic data-synthetic test
publisher Oxford University Press
url http://hdl.handle.net/10261/124227
http://dx.doi.org/10.13039/501100004837
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