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...

Full description

Main Authors: Boschini L., Ileana M., Alvarado Induni, Guillermo E., Rojas Quesada, Wilfredo
Format: Artículo
Language: Español
Published: Universidad de Costa Rica 2011
Online Access: http://revistas.ucr.ac.cr/index.php/geologica/article/view/12951
http://hdl.handle.net/10669/22382
Summary: 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.