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Authordc.contributor.authorLegrand Cabanes, Denis es_CL
Authordc.contributor.authorDelouis, B. es_CL
Authordc.contributor.authorDorbath, L. es_CL
Authordc.contributor.authorDavid, C. es_CL
Authordc.contributor.authorCampos Muñoz, Jaime es_CL
Authordc.contributor.authorMarquez, L. es_CL
Authordc.contributor.authorThompson, J. es_CL
Authordc.contributor.authorComte Selman, Diana es_CL
Admission datedc.date.accessioned2008-05-14T14:02:13Z
Available datedc.date.available2008-05-14T14:02:13Z
Publication datedc.date.issued2007es_CL
Cita de ítemdc.identifier.citationJOURNAL OF SOUTH AMERICAN EARTH SCIENCES Vol. 24 JUN 2007 1 58-68es_CL
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/124683
General notedc.descriptionPublicación ISIes_CL
Abstractdc.description.abstractThe July 24, 2001, M-w = 6.3 earthquake in Aroma, Chile, is one of the few moderately shallow earthquakes to occur recently in northern Chile. This study uses different seismological data (short-period, broadband, strong-motion) to locate the event and its corresponding aftershocks. In addition, it carefully constrains the focal depth using SP phase and the focal mechanism of the main-shock. Finally, a model of the strong-motion waveforms discriminates the activated fault plane among the two nodal planes. The main-shock fault plane solution obtained from the strong-motion analysis is (strike, dip, rake) = (14 degrees +/- 10 degrees, 53 degrees +/- 15 degrees, -163 degrees +/- 15 degrees), which indicates a rightlateral motion on an inclined fault, in agreement with the aftershock distribution, which also indicates a fault striking N 14 degrees E and dipping about 50 degrees E. (C) 2007 Elsevier Ltd. All rights reserved.es_CL
Lenguagedc.language.isoenes_CL
Keywordsdc.subjectcrustal seismicityes_CL
Area Temáticadc.subject.otherGeosciences, Multidisciplinaryes_CL
Títulodc.titleSource parameters of the M-w=6.3 Aroma crustal earthquake of July 24, 2001 (northern Chile), and its aftershock sequencees_CL
Document typedc.typeArtículo de revista


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