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Edmundo Schanze, Gilberto Leiva, Miguel Gómez and Alvaro Lopez
Engineering practitioners do not usually include soil-structure interactions in building design; rather, it is common to model and design foundations as embedded joints with joint?based reactions. In some cases, foundation structures are modeled as rigid...
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Catalina Quiñones-Bustos, Maria Teresa Bull and Claudio Oyarzo-Vera
This article proposes a vulnerability assessment model for evaluating buildings? expected seismic performance, as well as their vulnerability to tsunamis. The objective of this assessment is to provide appropriate information for decision makers regardin...
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Osvaldo Moreno Flores
Pág. 1 - 111
ResumenLa investigación tiene como propósito estudiar el alcance y contribución de la planificación y diseño del paisaje en la gestión de riesgos, adaptabilidad y resiliencia urbana de territorios afectados por desastres, tomando como caso de estudio el ...
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Jorge Quezada,Edilia Jaque,Nicole Catalán,Arturo Belmonte,Alfonso Fernández,Federico Isla
Pág. 295 - 315
The Tirúa-Mocha Island area (38.2°-38.4° S) in southern Chile has been affected by two megaearthquakes in only 50 years: the 1960 Mw=9.5 Valdivia earthquake and 2010 Mw=8.8 Maule earthquake. We studied in the field the vertical ground movements occurred ...
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Isabel Santibáñez,José Cembrano,Tiaren García-Pérez,Carlos Costa,Gonzalo Yáñez,Carlos Marquardt,Gloria Arancibia,Gabriel González
Pág. 32 - 65
The Chilean Andes, as a characteristic tectonic and geomorphological region, is a perfect location to unravel the geologic nature of seismic hazards. The Chilean segment of the Nazca-South American subduction zone has experienced mega-earthquakes with Mo...
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Marcelo Contreras, Andrés Tassara, Muriel Gerbault, Rodolfo Araya, Klaus Bataille
Pág. 247 - 262
We study interseismic deformation preceding the Mw8.8 2010 Maule earthquake by means of two-dimensional
finite-element modeling. Our goal is to gain insight into the fundamental factors controlling elastic strain build-up and
release in subduction zones,...
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Stefano Micheletti, Francisco Letelier Troncoso
Pág. pp. 17 - 58
Tras el terremoto y tsunami del 27 de febrero de 2010, la política de reconstrucción implementada por el gobierno de Chile favoreció el liderazgo de los agentes privados en el proceso y propuso soluciones estándar para todos los territorios, con un claro...
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Felipe Aguilera, Oscar Benavente, Francisco Gutiérrez, Jorge Romero, Ornella Saltori, Rodrigo González, Mariano Agusto, Alberto Caselli, Marcela Pizarro
Pág. 20 - 46
Planchón-Peteroa volcano started a renewed eruptive period between January 2010 and July 2011. This
eruptive period was characterized by the occurrence of 4 explosive eruptive phases, dominated by low-intensity phreatic
activity, which produced almost pe...
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Daniel Melnick,Marcos Moreno,Marco Cisternas,Andrés Tassara
Pág. 558 - 563
The Maule earthquake (Mw 8.8) that affected south-central Chile on February 27, 2010 was preceded by the 1835 event documented by FitzRoy and Darwin. The relation between both events has remained controversial. Fault slip in 2010 estimated by Lorito et a...
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Eduardo Ignacio Moscoso,Eduardo Contreras-Reyes
Pág. 564 - 572
Most of the recent published geodetic models of the 2010 Maule, Chile mega-thrust earthquake (Mw=8.8) show a pronounced slip maximum of 15-20 m offshore Iloca, indicating that co-seismic slip was largest north of the epicenter of the earthquake rupture a...
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