Upper crustal structure of Madeira Island revealed from ambient noise tomography
Autor(a) principal: | |
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Data de Publicação: | 2015 |
Outros Autores: | , , , , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
Texto Completo: | http://hdl.handle.net/10400.9/3027 |
Resumo: | We present the first image of the Madeira upper crustal structure, using ambient seismic noise tomography. 16 months of ambient noise, recorded in a dense network of 26 seismometers deployed across Madeira, allowed reconstructing Rayleigh wave Green's functions between receivers. Dispersion analysis was performed in the short period band from 1.0 to 4.0 s. Group velocity measurements were regionalized to obtain 2D tomographic images, with a lateral resolution of 2.0 km in central Madeira. Afterwards, the dispersion curves, extracted from each cell of the 2D group velocity maps, were inverted as a function of depth to obtain a 3D shear wave velocity model of the upper crust, from the surface to a depth of 2.0 km. The obtained 3D velocity model reveals features throughout the island that correlates well with surface geology and island evolution. |
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Upper crustal structure of Madeira Island revealed from ambient noise tomographyEstrutura geológicaTomografia sísmicaIlha da Madeira (Arquipélago da Madeira, Portugal)Arquipélago da Madeira (Portugal)We present the first image of the Madeira upper crustal structure, using ambient seismic noise tomography. 16 months of ambient noise, recorded in a dense network of 26 seismometers deployed across Madeira, allowed reconstructing Rayleigh wave Green's functions between receivers. Dispersion analysis was performed in the short period band from 1.0 to 4.0 s. Group velocity measurements were regionalized to obtain 2D tomographic images, with a lateral resolution of 2.0 km in central Madeira. Afterwards, the dispersion curves, extracted from each cell of the 2D group velocity maps, were inverted as a function of depth to obtain a 3D shear wave velocity model of the upper crust, from the surface to a depth of 2.0 km. The obtained 3D velocity model reveals features throughout the island that correlates well with surface geology and island evolution.ElsevierRepositório do LNEGMatos, CatarinaSilveira, GraçaMatias, LuísCaldeira, RitaRibeiro, Maria LuísaDias, NunoKrüger, FrankBento dos Santos, Telmo2016-06-29T21:00:26Z2015-062015-06-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10400.9/3027engMatos, Catarina... [et al.] - Upper crustal structure of Madeira Island revealed from ambient noise tomography. In: Journal of Volcanology and Geothermal Research, 298 (1 June 2015), p. 136-1450377-0273http://dx.doi.org./10.1016/j.jvolgeores.2015.03.017info:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2023-04-02T05:41:23Zoai:repositorio.lneg.pt:10400.9/3027Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T15:36:11.240130Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse |
dc.title.none.fl_str_mv |
Upper crustal structure of Madeira Island revealed from ambient noise tomography |
title |
Upper crustal structure of Madeira Island revealed from ambient noise tomography |
spellingShingle |
Upper crustal structure of Madeira Island revealed from ambient noise tomography Matos, Catarina Estrutura geológica Tomografia sísmica Ilha da Madeira (Arquipélago da Madeira, Portugal) Arquipélago da Madeira (Portugal) |
title_short |
Upper crustal structure of Madeira Island revealed from ambient noise tomography |
title_full |
Upper crustal structure of Madeira Island revealed from ambient noise tomography |
title_fullStr |
Upper crustal structure of Madeira Island revealed from ambient noise tomography |
title_full_unstemmed |
Upper crustal structure of Madeira Island revealed from ambient noise tomography |
title_sort |
Upper crustal structure of Madeira Island revealed from ambient noise tomography |
author |
Matos, Catarina |
author_facet |
Matos, Catarina Silveira, Graça Matias, Luís Caldeira, Rita Ribeiro, Maria Luísa Dias, Nuno Krüger, Frank Bento dos Santos, Telmo |
author_role |
author |
author2 |
Silveira, Graça Matias, Luís Caldeira, Rita Ribeiro, Maria Luísa Dias, Nuno Krüger, Frank Bento dos Santos, Telmo |
author2_role |
author author author author author author author |
dc.contributor.none.fl_str_mv |
Repositório do LNEG |
dc.contributor.author.fl_str_mv |
Matos, Catarina Silveira, Graça Matias, Luís Caldeira, Rita Ribeiro, Maria Luísa Dias, Nuno Krüger, Frank Bento dos Santos, Telmo |
dc.subject.por.fl_str_mv |
Estrutura geológica Tomografia sísmica Ilha da Madeira (Arquipélago da Madeira, Portugal) Arquipélago da Madeira (Portugal) |
topic |
Estrutura geológica Tomografia sísmica Ilha da Madeira (Arquipélago da Madeira, Portugal) Arquipélago da Madeira (Portugal) |
description |
We present the first image of the Madeira upper crustal structure, using ambient seismic noise tomography. 16 months of ambient noise, recorded in a dense network of 26 seismometers deployed across Madeira, allowed reconstructing Rayleigh wave Green's functions between receivers. Dispersion analysis was performed in the short period band from 1.0 to 4.0 s. Group velocity measurements were regionalized to obtain 2D tomographic images, with a lateral resolution of 2.0 km in central Madeira. Afterwards, the dispersion curves, extracted from each cell of the 2D group velocity maps, were inverted as a function of depth to obtain a 3D shear wave velocity model of the upper crust, from the surface to a depth of 2.0 km. The obtained 3D velocity model reveals features throughout the island that correlates well with surface geology and island evolution. |
publishDate |
2015 |
dc.date.none.fl_str_mv |
2015-06 2015-06-01T00:00:00Z 2016-06-29T21:00:26Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://hdl.handle.net/10400.9/3027 |
url |
http://hdl.handle.net/10400.9/3027 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
Matos, Catarina... [et al.] - Upper crustal structure of Madeira Island revealed from ambient noise tomography. In: Journal of Volcanology and Geothermal Research, 298 (1 June 2015), p. 136-145 0377-0273 http://dx.doi.org./10.1016/j.jvolgeores.2015.03.017 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Elsevier |
publisher.none.fl_str_mv |
Elsevier |
dc.source.none.fl_str_mv |
reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação instacron:RCAAP |
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Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
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RCAAP |
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RCAAP |
reponame_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
collection |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
repository.name.fl_str_mv |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
repository.mail.fl_str_mv |
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1799130227163529216 |