Seismic Source Directivity From Doppler Effect Analysis, Part II: Application To The Zemmouri-Boumerdes (Algeria) Earthquake of May 21st, 2003, Mw=6.8

Detalhes bibliográficos
Autor(a) principal: Caldeira, B
Data de Publicação: 2004
Outros Autores: Bezzeghoud, M, Borges, JF
Tipo de documento: Artigo de conferência
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10174/6676
Resumo: On May 21, 2003, the Eastern part of Algiers was struck by an earthquake (Mw=6.8) that injured 11.455 people and caused serious damage in cities close the hypocenter. The purpose of this work is to analyse the rupture directivity of this event using a Doppler Effect approach. The inversion method developed (DIRDOP) (Caldeira et al., 2004) allows an estimation of the rupture direction and velocity from a collection of time pulses, extracted from body waveforms or a relative source time function (RSTF). This seismic data has been downloaded from the IRIS consortium and has a reasonable azimuthal coverage. We have used 30 teleseismic broadband body wave data and 6 relative RSTF obtained from the deconvolution in the time domain (Borges, 2003) using the synthetic Green functions. These are calculated using the Haskell propagator matrix. The results show a bilateral rupture in the E-W direction. In the first 5 seconds the rupture propagates from the epicentre toward the East (N87oE +-13o) with an average velocity of 2.9 0.31km/s. In the last 10 seconds the rupture propagates with the same velocity but in the opposite direction (S84W+- 14o). Both results are coherent with the focal mechanism (strike=64o, dip=50o, rake=83o) and the seismic source obtained elsewhere (Bezzeghoud et al., 2004). REFERENCES Bezzeghoud M., B. Caldeira, J.F. Borges, A. Ayadi and E. Buforn. The Zemmouri-Boumerdes earthquake of may 21st, 2003, mw=6.8: source parameters and rupture propagation study from teleseismic data. XXIX General Assembly of the European Seis- mological Commission (ESC), 12-17 September, Potsdam, this issue. Borges J. F., 2003. Fonte sísmica em Portugal – algumas implicações na geodinâmica da região Açores-Gibraltar. PhD thesis, Universidade de Évora, p. 387 Caldeira B., M. Bezzeghoud and J. Borges, 2004. Seismic source directivity from Doppler effect analysis, part I: Theory. XXIX General Assembly of the European Seismological Commission (ESC), 12-17 September, Potsdam, this issue
id RCAP_4253c0665e951aed9202b5573f8a7f24
oai_identifier_str oai:dspace.uevora.pt:10174/6676
network_acronym_str RCAP
network_name_str Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
repository_id_str 7160
spelling Seismic Source Directivity From Doppler Effect Analysis, Part II: Application To The Zemmouri-Boumerdes (Algeria) Earthquake of May 21st, 2003, Mw=6.8Rupture ProcesseDirectivityOn May 21, 2003, the Eastern part of Algiers was struck by an earthquake (Mw=6.8) that injured 11.455 people and caused serious damage in cities close the hypocenter. The purpose of this work is to analyse the rupture directivity of this event using a Doppler Effect approach. The inversion method developed (DIRDOP) (Caldeira et al., 2004) allows an estimation of the rupture direction and velocity from a collection of time pulses, extracted from body waveforms or a relative source time function (RSTF). This seismic data has been downloaded from the IRIS consortium and has a reasonable azimuthal coverage. We have used 30 teleseismic broadband body wave data and 6 relative RSTF obtained from the deconvolution in the time domain (Borges, 2003) using the synthetic Green functions. These are calculated using the Haskell propagator matrix. The results show a bilateral rupture in the E-W direction. In the first 5 seconds the rupture propagates from the epicentre toward the East (N87oE +-13o) with an average velocity of 2.9 0.31km/s. In the last 10 seconds the rupture propagates with the same velocity but in the opposite direction (S84W+- 14o). Both results are coherent with the focal mechanism (strike=64o, dip=50o, rake=83o) and the seismic source obtained elsewhere (Bezzeghoud et al., 2004). REFERENCES Bezzeghoud M., B. Caldeira, J.F. Borges, A. Ayadi and E. Buforn. The Zemmouri-Boumerdes earthquake of may 21st, 2003, mw=6.8: source parameters and rupture propagation study from teleseismic data. XXIX General Assembly of the European Seis- mological Commission (ESC), 12-17 September, Potsdam, this issue. Borges J. F., 2003. Fonte sísmica em Portugal – algumas implicações na geodinâmica da região Açores-Gibraltar. PhD thesis, Universidade de Évora, p. 387 Caldeira B., M. Bezzeghoud and J. Borges, 2004. Seismic source directivity from Doppler effect analysis, part I: Theory. XXIX General Assembly of the European Seismological Commission (ESC), 12-17 September, Potsdam, this issueXXIX General Assembly of the European Seismological Commission (ESC), 13-17 September, Potsdam, Germany.2012-12-07T17:39:48Z2012-12-072004-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjecthttp://hdl.handle.net/10174/6676http://hdl.handle.net/10174/6676engCaldeira B., M. Bezzeghoud and J. F. Borges, 2004. Seismic Source Directivity From Doppler Effect Analysis, Part II: Application To The Zemmouri-Boumerdes (Algeria) Earthquake of May 21st, 2003, Mw=6.8. XXIX General Assembly of the European Seismological Commission (ESC), 13-17 September, Potsdam, Germany.naonaonaobafcc@uevora.ptmourad@uevora.ptjborges@uevora.pt249Caldeira, BBezzeghoud, MBorges, JFinfo: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:RCAAP2024-01-03T18:45:58Zoai:dspace.uevora.pt:10174/6676Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T01:01:14.067862Repositório 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 Seismic Source Directivity From Doppler Effect Analysis, Part II: Application To The Zemmouri-Boumerdes (Algeria) Earthquake of May 21st, 2003, Mw=6.8
title Seismic Source Directivity From Doppler Effect Analysis, Part II: Application To The Zemmouri-Boumerdes (Algeria) Earthquake of May 21st, 2003, Mw=6.8
spellingShingle Seismic Source Directivity From Doppler Effect Analysis, Part II: Application To The Zemmouri-Boumerdes (Algeria) Earthquake of May 21st, 2003, Mw=6.8
Caldeira, B
Rupture Processe
Directivity
title_short Seismic Source Directivity From Doppler Effect Analysis, Part II: Application To The Zemmouri-Boumerdes (Algeria) Earthquake of May 21st, 2003, Mw=6.8
title_full Seismic Source Directivity From Doppler Effect Analysis, Part II: Application To The Zemmouri-Boumerdes (Algeria) Earthquake of May 21st, 2003, Mw=6.8
title_fullStr Seismic Source Directivity From Doppler Effect Analysis, Part II: Application To The Zemmouri-Boumerdes (Algeria) Earthquake of May 21st, 2003, Mw=6.8
title_full_unstemmed Seismic Source Directivity From Doppler Effect Analysis, Part II: Application To The Zemmouri-Boumerdes (Algeria) Earthquake of May 21st, 2003, Mw=6.8
title_sort Seismic Source Directivity From Doppler Effect Analysis, Part II: Application To The Zemmouri-Boumerdes (Algeria) Earthquake of May 21st, 2003, Mw=6.8
author Caldeira, B
author_facet Caldeira, B
Bezzeghoud, M
Borges, JF
author_role author
author2 Bezzeghoud, M
Borges, JF
author2_role author
author
dc.contributor.author.fl_str_mv Caldeira, B
Bezzeghoud, M
Borges, JF
dc.subject.por.fl_str_mv Rupture Processe
Directivity
topic Rupture Processe
Directivity
description On May 21, 2003, the Eastern part of Algiers was struck by an earthquake (Mw=6.8) that injured 11.455 people and caused serious damage in cities close the hypocenter. The purpose of this work is to analyse the rupture directivity of this event using a Doppler Effect approach. The inversion method developed (DIRDOP) (Caldeira et al., 2004) allows an estimation of the rupture direction and velocity from a collection of time pulses, extracted from body waveforms or a relative source time function (RSTF). This seismic data has been downloaded from the IRIS consortium and has a reasonable azimuthal coverage. We have used 30 teleseismic broadband body wave data and 6 relative RSTF obtained from the deconvolution in the time domain (Borges, 2003) using the synthetic Green functions. These are calculated using the Haskell propagator matrix. The results show a bilateral rupture in the E-W direction. In the first 5 seconds the rupture propagates from the epicentre toward the East (N87oE +-13o) with an average velocity of 2.9 0.31km/s. In the last 10 seconds the rupture propagates with the same velocity but in the opposite direction (S84W+- 14o). Both results are coherent with the focal mechanism (strike=64o, dip=50o, rake=83o) and the seismic source obtained elsewhere (Bezzeghoud et al., 2004). REFERENCES Bezzeghoud M., B. Caldeira, J.F. Borges, A. Ayadi and E. Buforn. The Zemmouri-Boumerdes earthquake of may 21st, 2003, mw=6.8: source parameters and rupture propagation study from teleseismic data. XXIX General Assembly of the European Seis- mological Commission (ESC), 12-17 September, Potsdam, this issue. Borges J. F., 2003. Fonte sísmica em Portugal – algumas implicações na geodinâmica da região Açores-Gibraltar. PhD thesis, Universidade de Évora, p. 387 Caldeira B., M. Bezzeghoud and J. Borges, 2004. Seismic source directivity from Doppler effect analysis, part I: Theory. XXIX General Assembly of the European Seismological Commission (ESC), 12-17 September, Potsdam, this issue
publishDate 2004
dc.date.none.fl_str_mv 2004-01-01T00:00:00Z
2012-12-07T17:39:48Z
2012-12-07
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/conferenceObject
format conferenceObject
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://hdl.handle.net/10174/6676
http://hdl.handle.net/10174/6676
url http://hdl.handle.net/10174/6676
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Caldeira B., M. Bezzeghoud and J. F. Borges, 2004. Seismic Source Directivity From Doppler Effect Analysis, Part II: Application To The Zemmouri-Boumerdes (Algeria) Earthquake of May 21st, 2003, Mw=6.8. XXIX General Assembly of the European Seismological Commission (ESC), 13-17 September, Potsdam, Germany.
nao
nao
nao
bafcc@uevora.pt
mourad@uevora.pt
jborges@uevora.pt
249
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv XXIX General Assembly of the European Seismological Commission (ESC), 13-17 September, Potsdam, Germany.
publisher.none.fl_str_mv XXIX General Assembly of the European Seismological Commission (ESC), 13-17 September, Potsdam, Germany.
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
instname_str Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação
instacron_str RCAAP
institution 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
_version_ 1799136495681929216