Analysis of October 23 (Mw 7.2) and November 9 (Mw 5.6), 2011 Van Earthquakes Using Long-Term GNSS Time Series

The eastern Anatolia provides one of the best examples of an area of rapid deformation and intense contraction that is the consequence of an active continental collision between the Arabian and Eurasian plates leading to large and devastating earthquakes. The latest evidence of the active tectonism...

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Autores:
Tiryakioglu, Ibrahim
Yavasoglu, Hakan
Ugur, Mehmet Ali Ugur
Ozkaymak, Caglar
Yilmaz, Mustafa
Kocaoglu, Hasan
Turgut, Bayram
Tipo de recurso:
Article of journal
Fecha de publicación:
2017
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/63573
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/63573
http://bdigital.unal.edu.co/64019/
Palabra clave:
55 Ciencias de la tierra / Earth sciences and geology
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openAccess
License
Atribución-NoComercial 4.0 Internacional
id UNACIONAL2_aaea0359b93fcc9ec43609dd6336b257
oai_identifier_str oai:repositorio.unal.edu.co:unal/63573
network_acronym_str UNACIONAL2
network_name_str Universidad Nacional de Colombia
repository_id_str
dc.title.spa.fl_str_mv Analysis of October 23 (Mw 7.2) and November 9 (Mw 5.6), 2011 Van Earthquakes Using Long-Term GNSS Time Series
title Analysis of October 23 (Mw 7.2) and November 9 (Mw 5.6), 2011 Van Earthquakes Using Long-Term GNSS Time Series
spellingShingle Analysis of October 23 (Mw 7.2) and November 9 (Mw 5.6), 2011 Van Earthquakes Using Long-Term GNSS Time Series
55 Ciencias de la tierra / Earth sciences and geology
title_short Analysis of October 23 (Mw 7.2) and November 9 (Mw 5.6), 2011 Van Earthquakes Using Long-Term GNSS Time Series
title_full Analysis of October 23 (Mw 7.2) and November 9 (Mw 5.6), 2011 Van Earthquakes Using Long-Term GNSS Time Series
title_fullStr Analysis of October 23 (Mw 7.2) and November 9 (Mw 5.6), 2011 Van Earthquakes Using Long-Term GNSS Time Series
title_full_unstemmed Analysis of October 23 (Mw 7.2) and November 9 (Mw 5.6), 2011 Van Earthquakes Using Long-Term GNSS Time Series
title_sort Analysis of October 23 (Mw 7.2) and November 9 (Mw 5.6), 2011 Van Earthquakes Using Long-Term GNSS Time Series
dc.creator.fl_str_mv Tiryakioglu, Ibrahim
Yavasoglu, Hakan
Ugur, Mehmet Ali Ugur
Ozkaymak, Caglar
Yilmaz, Mustafa
Kocaoglu, Hasan
Turgut, Bayram
dc.contributor.author.spa.fl_str_mv Tiryakioglu, Ibrahim
Yavasoglu, Hakan
Ugur, Mehmet Ali Ugur
Ozkaymak, Caglar
Yilmaz, Mustafa
Kocaoglu, Hasan
Turgut, Bayram
dc.subject.ddc.spa.fl_str_mv 55 Ciencias de la tierra / Earth sciences and geology
topic 55 Ciencias de la tierra / Earth sciences and geology
description The eastern Anatolia provides one of the best examples of an area of rapid deformation and intense contraction that is the consequence of an active continental collision between the Arabian and Eurasian plates leading to large and devastating earthquakes. The latest evidence of the active tectonism in the region is revealed by two remarkable seismic events; Van-Tabanli (Mw 7.2, October 23, 2011) and Van-Edremit (Mw 5.6, November 9, 2011) earthquakes. The study of the earthquake cycle and observation of geodetic and seismic deformation in this region is very important to hazard assessments. In this study, the inter-seismic, co-seismic, and post-seismic movements caused by the above-mentioned earthquakes were investigated using the time series of 2300 days of Global Navigation Satellite Systems (GNSS) observations of the local stations selected from the network of the Continuously Operating Reference Stations, Turkey (CORS-TR). For the inter-seismic period, approximately 1100 daily data were obtained from 21 CORS-TR stations (prior to the earthquakes between October 1, 2008 and October 23, 2011) and evaluated using the GAMIT/GLOBK software. The behaviour of these stations was investigated by processing 1 Hz data from the GNSS stations during the earthquakes on the GAMIT/TRACK software. In addition to October 23 and November 9, the GNSS data on one day before and after the earthquakes was assessed to determine co-seismic deformations. During the October 23 earthquake, hanging-wall deformation of about 60 mm was detected in the SW direction at the MURA station. However, at the VAAN station, deformation of 200 mm (value predicted by time series) was observed in the footwall block in the NW direction. There were not any significant changes at the stations during the November 9 earthquake. For the post-seismic period, the GNSS data from 2012 to 2015 was evaluated. According to the observations, post-seismic deformation continued at the stations close to the epicenter of the earthquake.
publishDate 2017
dc.date.issued.spa.fl_str_mv 2017-07-01
dc.date.accessioned.spa.fl_str_mv 2019-07-02T21:54:50Z
dc.date.available.spa.fl_str_mv 2019-07-02T21:54:50Z
dc.type.spa.fl_str_mv Artículo de revista
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dc.identifier.issn.spa.fl_str_mv ISSN: 2339-3459
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identifier_str_mv ISSN: 2339-3459
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dc.relation.spa.fl_str_mv https://revistas.unal.edu.co/index.php/esrj/article/view/62812
dc.relation.ispartof.spa.fl_str_mv Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research Journal
Earth Sciences Research Journal
dc.relation.references.spa.fl_str_mv Tiryakioglu, Ibrahim and Yavasoglu, Hakan and Ugur, Mehmet Ali Ugur and Ozkaymak, Caglar and Yilmaz, Mustafa and Kocaoglu, Hasan and Turgut, Bayram (2017) Analysis of October 23 (Mw 7.2) and November 9 (Mw 5.6), 2011 Van Earthquakes Using Long-Term GNSS Time Series. Earth Sciences Research Journal, 21 (3). pp. 147-156. ISSN 2339-3459
dc.rights.spa.fl_str_mv Derechos reservados - Universidad Nacional de Colombia
dc.rights.coar.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.rights.license.spa.fl_str_mv Atribución-NoComercial 4.0 Internacional
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dc.rights.accessrights.spa.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv Atribución-NoComercial 4.0 Internacional
Derechos reservados - Universidad Nacional de Colombia
http://creativecommons.org/licenses/by-nc/4.0/
http://purl.org/coar/access_right/c_abf2
eu_rights_str_mv openAccess
dc.format.mimetype.spa.fl_str_mv application/pdf
dc.publisher.spa.fl_str_mv Universidad Nacional de Colombia - Sede Bogotá - Facultad de Ciencias - Departamento de Geociencia
institution Universidad Nacional de Colombia
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spelling Atribución-NoComercial 4.0 InternacionalDerechos reservados - Universidad Nacional de Colombiahttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Tiryakioglu, Ibrahimca4f8b0c-2dc4-4574-af97-7d205680b6fc300Yavasoglu, Hakan023dbe7a-c2ae-4f86-a41f-d8082ea3cb03300Ugur, Mehmet Ali Ugurb7dbbd1f-0ae4-4d6c-a496-d13dbc6f26cc300Ozkaymak, Caglarbc269885-9fd3-47e8-a76a-f830c9100445300Yilmaz, Mustafacb0ceb9f-2d37-4c49-8725-1c51e498c815300Kocaoglu, Hasan14efda09-97ce-4c01-be2c-352fe2333352300Turgut, Bayramc815ec71-2252-4e69-9ee9-0474d82727703002019-07-02T21:54:50Z2019-07-02T21:54:50Z2017-07-01ISSN: 2339-3459https://repositorio.unal.edu.co/handle/unal/63573http://bdigital.unal.edu.co/64019/The eastern Anatolia provides one of the best examples of an area of rapid deformation and intense contraction that is the consequence of an active continental collision between the Arabian and Eurasian plates leading to large and devastating earthquakes. The latest evidence of the active tectonism in the region is revealed by two remarkable seismic events; Van-Tabanli (Mw 7.2, October 23, 2011) and Van-Edremit (Mw 5.6, November 9, 2011) earthquakes. The study of the earthquake cycle and observation of geodetic and seismic deformation in this region is very important to hazard assessments. In this study, the inter-seismic, co-seismic, and post-seismic movements caused by the above-mentioned earthquakes were investigated using the time series of 2300 days of Global Navigation Satellite Systems (GNSS) observations of the local stations selected from the network of the Continuously Operating Reference Stations, Turkey (CORS-TR). For the inter-seismic period, approximately 1100 daily data were obtained from 21 CORS-TR stations (prior to the earthquakes between October 1, 2008 and October 23, 2011) and evaluated using the GAMIT/GLOBK software. The behaviour of these stations was investigated by processing 1 Hz data from the GNSS stations during the earthquakes on the GAMIT/TRACK software. In addition to October 23 and November 9, the GNSS data on one day before and after the earthquakes was assessed to determine co-seismic deformations. During the October 23 earthquake, hanging-wall deformation of about 60 mm was detected in the SW direction at the MURA station. However, at the VAAN station, deformation of 200 mm (value predicted by time series) was observed in the footwall block in the NW direction. There were not any significant changes at the stations during the November 9 earthquake. For the post-seismic period, the GNSS data from 2012 to 2015 was evaluated. According to the observations, post-seismic deformation continued at the stations close to the epicenter of the earthquake.Anatolia oriental provee uno de los mejores ejemplos de un área de rápida deformación e intensa contracción, consecuencia de una colisión continental activa entre la placa Arábiga y la Euroasiática, lo que causa grandes y devastadores terremotos. Dos notables terremotos son evidencia de la actividad tectónica de la región: los terremotos Van-Tabanli (7.2 Mw. 23 de octubre de 2011) y Van-Edremit (5.6 Mw, 9 de noviembre de 2011). El estudio del ciclo sísmico y la observación de las deformaciones geodésicas y sísmicas en esta región es fundamental para la evaluación de riesgo. En este estudio, se investiga las fases inter-, co- y post-sísmicas asociados a estos terremotos a través de 2300 días de observaciones del Sistema Global de Navegación por Satélite (GNSS, por sus siglas en inglés) de estaciones locales seleccionadas de la red de Estaciones de Referencia de Funcionamiento Continuo en Turquía (CORS-TR). Para el periodo intersísmico se obtuvieron aproximadamente 1100 datos diarios de 21 estaciones CORS-TR (anteriores a los terremotos entre el 1 de octubre de 2008 y el 23 de octubre de 2011) y evaluados con el software GAMIT/GBLOK. El comportamiento co-sísmico fue investigado procesando datos de 1 Hz de las estaciones GNSS durante los terremotos en el software GAMIT/TRACK. Adicionalmente se evaluaron datos del GNSS un día antes y un día después de los terremotos para determinar las deformaciones cosísmicas. Durante el terremoto del 23 de octubre, en el bloque colgante se detectó una deformación de 60 mm en dirección SW (estación MURA). En la estación VAAN en el bloque yacente se observó una deformación de 200 mm en dirección NW (valor predicho por series temporales). Durtante el terremoto del 9 de Noviembre no se observó cambios significativos. Para la fase post-sísmica se evaluaron los datos de la GNSS del 2012 al 2015. Según las observaciones, la deformación postsísmica continuó en las estaciones cercanas al epicentro del terremoto.application/pdfspaUniversidad Nacional de Colombia - Sede Bogotá - Facultad de Ciencias - Departamento de Geocienciahttps://revistas.unal.edu.co/index.php/esrj/article/view/62812Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research JournalEarth Sciences Research JournalTiryakioglu, Ibrahim and Yavasoglu, Hakan and Ugur, Mehmet Ali Ugur and Ozkaymak, Caglar and Yilmaz, Mustafa and Kocaoglu, Hasan and Turgut, Bayram (2017) Analysis of October 23 (Mw 7.2) and November 9 (Mw 5.6), 2011 Van Earthquakes Using Long-Term GNSS Time Series. Earth Sciences Research Journal, 21 (3). pp. 147-156. ISSN 2339-345955 Ciencias de la tierra / Earth sciences and geologyAnalysis of October 23 (Mw 7.2) and November 9 (Mw 5.6), 2011 Van Earthquakes Using Long-Term GNSS Time SeriesArtículo de revistainfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/ARTORIGINAL62812-352571-2-PB.pdfapplication/pdf4297446https://repositorio.unal.edu.co/bitstream/unal/63573/1/62812-352571-2-PB.pdfa3dd875ee3bc1096f6093231259f0e6cMD51THUMBNAIL62812-352571-2-PB.pdf.jpg62812-352571-2-PB.pdf.jpgGenerated Thumbnailimage/jpeg8251https://repositorio.unal.edu.co/bitstream/unal/63573/2/62812-352571-2-PB.pdf.jpg976743ae37b285b58edec14c4828914eMD52unal/63573oai:repositorio.unal.edu.co:unal/635732023-04-22 23:05:24.206Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co