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- W2320060388 abstract "PreviousNext No Access12th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 15–18 August 2011The Mara Rosa 5.0 mb earthquake and aftershock activityAuthors: Lucas V. BarrosCristiano N. ChimpliganondMônica G. Von HuelsenGeorge Sand FrançaDaniel de Farias CaixetaDiogo Farrapo AlbuquerqueLucas V. BarrosInstituto de Geociências, Observatório Sismológico, Universidade de BrasíliaSearch for more papers by this author, Cristiano N. ChimpliganondInstituto de Geociências, Observatório Sismológico, Universidade de BrasíliaSearch for more papers by this author, Mônica G. Von HuelsenInstituto de Geociências, Observatório Sismológico, Universidade de BrasíliaSearch for more papers by this author, George Sand FrançaInstituto de Geociências, Observatório Sismológico, Universidade de BrasíliaSearch for more papers by this author, Daniel de Farias CaixetaInstituto de Geociências, Observatório Sismológico, Universidade de BrasíliaSearch for more papers by this author, and Diogo Farrapo AlbuquerqueInstituto de Geociências, Observatório Sismológico, Universidade de BrasíliaSearch for more papers by this authorhttps://doi.org/10.1190/sbgf2011-406 SectionsAboutPDF/ePub ToolsAdd to favoritesDownload CitationsTrack CitationsPermissions ShareFacebookTwitterLinked InRedditEmail Abstract In October 8th, 2010, a 5.0 mb (MMI VI) earthquake occurred close to Mara Rosa, in the North of Goiás State, Brazil, in an area where previous low magnitude seismicity had been observed. However, this was the biggest earthquake ever detected in this area, felt up to 300 km away from the epicenter. This event may be associated with reactivation of some geological fault of the Transbrazilian Lineament (TL), since the aftershock activity observed from October of 2010 to January of 2011 indicates a SW-NE trending fault, parallel to TL and consistent with one nodal plane of the composite focal mechanism solution. This work presents preliminary results of studies on seismicity, geology and geophysics conducted by the Seismological Observatory of the University of Brasília on the main earthquake of Mara Rosa of October 8th, 2010 and aftershock activity detected by a local seismic network. Keywords: earthquake, aftershock, transbrazilian lineament, faults, seismicPermalink: https://doi.org/10.1190/sbgf2011-406FiguresReferencesRelatedDetailsCited ByThe 2012–2013 Montes Claros earthquake series in the São Francisco Craton, Brazil: new evidence for non-uniform intraplate stresses in mid-plate South America11 November 2014 | Geophysical Journal International, Vol. 200, No. 1Seismic source parameters of local micro earthquake in Goiás State Brazil by waveform inversionJuraci Mário de Carvalho and Lucas Vieira Barros9 January 2014 12th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 15–18 August 2011ISSN (online):2159-6832Copyright: 2011 Pages: 2223 publication data© 2011 Published in electronic format with permission by the Brazilian Geophysical SocietyPublisher:Society of Exploration Geophysicists HistoryPublished: 13 Mar 2014 CITATION INFORMATION Lucas V. Barros, Cristiano N. Chimpliganond, Mônica G. Von Huelsen, George Sand França, Daniel de Farias Caixeta, and Diogo Farrapo Albuquerque, (2011), The Mara Rosa 5.0 mb earthquake and aftershock activity, SEG Global Meeting Abstracts : 1970-1974. https://doi.org/10.1190/sbgf2011-406 Plain-Language Summary Keywordsearthquakeaftershocktransbrazilian lineamentfaultsseismicPDF DownloadLoading ..." @default.
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