Study on the limitations of travel-time inversion applied to sub-basalt imaging

The difficulties of seismic imaging beneath high velocity structures are widely recognised. In this setting, theoretical analysis of synthetic wide-angle seismic reflection data indicates that velocity models are not well constrained. A two-dimensional velocity model was built to simulate a simplifi...

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Main Authors: I. Flecha, R. Carbonell, R. W. Hobbs
Format: Article
Language:English
Published: Copernicus Publications 2013-12-01
Series:Solid Earth
Online Access:http://www.solid-earth.net/4/543/2013/se-4-543-2013.pdf
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spelling doaj-a81e0cafbfa94e4b95d9dc100046066e2020-11-25T00:50:11ZengCopernicus PublicationsSolid Earth1869-95101869-95292013-12-014254355410.5194/se-4-543-2013Study on the limitations of travel-time inversion applied to sub-basalt imagingI. Flecha0R. Carbonell1R. W. Hobbs2Departament de Estructura i Dinàmica de la Terra, Institut de Ciències de la Terra Jaume Almera-ICTJA-CSIC, C/ Lluís Solé i Sabarís s/n, 08028, Barcelona, SpainDepartament de Estructura i Dinàmica de la Terra, Institut de Ciències de la Terra Jaume Almera-ICTJA-CSIC, C/ Lluís Solé i Sabarís s/n, 08028, Barcelona, SpainDepartment of Earth Sciences, University of Durham, Durham DH1 3LE, UKThe difficulties of seismic imaging beneath high velocity structures are widely recognised. In this setting, theoretical analysis of synthetic wide-angle seismic reflection data indicates that velocity models are not well constrained. A two-dimensional velocity model was built to simulate a simplified structural geometry given by a basaltic wedge placed within a sedimentary sequence. This model reproduces the geological setting in areas of special interest for the oil industry as the Faroe-Shetland Basin. A wide-angle synthetic dataset was calculated on this model using an elastic finite difference scheme. This dataset provided travel times for tomographic inversions. Results show that the original model can not be completely resolved without considering additional information. The resolution of nonlinear inversions lacks a functional mathematical relationship, therefore, statistical approaches are required. Stochastic tests based on Metropolis techniques support the need of additional information to properly resolve sub-basalt structures.http://www.solid-earth.net/4/543/2013/se-4-543-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author I. Flecha
R. Carbonell
R. W. Hobbs
spellingShingle I. Flecha
R. Carbonell
R. W. Hobbs
Study on the limitations of travel-time inversion applied to sub-basalt imaging
Solid Earth
author_facet I. Flecha
R. Carbonell
R. W. Hobbs
author_sort I. Flecha
title Study on the limitations of travel-time inversion applied to sub-basalt imaging
title_short Study on the limitations of travel-time inversion applied to sub-basalt imaging
title_full Study on the limitations of travel-time inversion applied to sub-basalt imaging
title_fullStr Study on the limitations of travel-time inversion applied to sub-basalt imaging
title_full_unstemmed Study on the limitations of travel-time inversion applied to sub-basalt imaging
title_sort study on the limitations of travel-time inversion applied to sub-basalt imaging
publisher Copernicus Publications
series Solid Earth
issn 1869-9510
1869-9529
publishDate 2013-12-01
description The difficulties of seismic imaging beneath high velocity structures are widely recognised. In this setting, theoretical analysis of synthetic wide-angle seismic reflection data indicates that velocity models are not well constrained. A two-dimensional velocity model was built to simulate a simplified structural geometry given by a basaltic wedge placed within a sedimentary sequence. This model reproduces the geological setting in areas of special interest for the oil industry as the Faroe-Shetland Basin. A wide-angle synthetic dataset was calculated on this model using an elastic finite difference scheme. This dataset provided travel times for tomographic inversions. Results show that the original model can not be completely resolved without considering additional information. The resolution of nonlinear inversions lacks a functional mathematical relationship, therefore, statistical approaches are required. Stochastic tests based on Metropolis techniques support the need of additional information to properly resolve sub-basalt structures.
url http://www.solid-earth.net/4/543/2013/se-4-543-2013.pdf
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