El terremoto de Buenavista de Pérez Zeledón (julio 3, 1983): evidencia de una fuente sismogénica intraplaca desconocida en Costa Rica

Seismological and neotonic aspects of the Buenavista fault that generated the earthquake of the same name (July 3, 1983); h- 14 km mb- 5.7 and Ms- 6.1) are analized. This earthquake affected an area of 400 km2 corresponding to the zone surrounded by the VIII isosists (MM) in the northern region of S...

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Autores Principales: Boschini L., Ileana M., Alvarado Induni, Guillermo E., Rojas Quesada, Wilfredo
Formato: Artículo
Idioma: Español
Publicado: Universidad de Costa Rica 2011
Acceso en línea: http://revistas.ucr.ac.cr/index.php/geologica/article/view/12951
http://hdl.handle.net/10669/22382
Sumario: Seismological and neotonic aspects of the Buenavista fault that generated the earthquake of the same name (July 3, 1983); h- 14 km mb- 5.7 and Ms- 6.1) are analized. This earthquake affected an area of 400 km2 corresponding to the zone surrounded by the VIII isosists (MM) in the northern region of San Isidro del General, Costa Rica.