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Autor Staller, A. |
Documentos disponibles escritos por este autor (5)
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Fernández, J. ; Gónzalez Matesanz, F. J. ; Prieto, J. F. ; Rodríguez Velasco, Gema ; Staller, A. ; Alonso Medina, A. ; Charco Romero, María | Birkhäuser | 2004This paper describes design, observation methodology, results and interpretation of the GPS surveys conducted in the areas of the N-W of Tenerife where deformation was detected using InSAR. To avoid undesirable antenna positioning errors in the [...]texto impreso
Alonso Henar, Jorge ; Benito, Belén ; Staller, A. ; Álvarez Gómez, José Antonio ; Martínez Díaz, José J. ; Canora Catalán, Carolina | Elsevier | 2018-09-04During the last years, several crustal seismic sources have been proposed in El Salvador; however, the actual destructive potential of these proposals has not been revealed yet. Here we present several seismic scenarios related with the main cru[...]texto impreso
Alonso Henar, Jorge ; Benito, Belén ; Staller, A. ; Álvarez Gómez, José Antonio ; Martínez Díaz, José J. ; Canora Catalán, Carolina | Elsevier | 2018-10We present a map and a data set containing information about intra-plate seismic sources in El Salvador. These are the results of the field campaigns and data analysis carried out by the research group of Planetary Geodinamics, Active Tectonics [...]texto impreso
Alonso-Henar, Jorge ; Staller, A. ; Martínez Díaz, José J. ; Benito, Belén ; Álvarez Gómez, José Antonio ; Canora Catalán, Carolina | Copernicus Publications; European Geosciences Union | 2014El Salvador is located at the pacific active margin of Central America, here, the subduction of the Cocos Plate under the Caribbean Plate at a rate of 80 mm/yr is the main seismic source. Although the seismic sources located in the Central Ameri[...]texto impreso
Canora Catalán, Carolina ; Martínez Díaz, José J. ; Villamor Pérez, María Pilar ; Staller, A. ; Berryman, K.R. ; Álvarez Gómez, José Antonio ; Capote del Villar, Ramón ; Díaz Flores, Manuel Roberto | Universidad Complutense de Madrid | 2014The El Salvador Fault Zone, firstly identified after the 13th February 2001 Mw 6.6 El Salvador earthquake, is a 150 km long, 20 km wide right-lateral strike-slip fault system. Ruptures along the ESFZ are thought to be responsible for most of the[...]