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Resultats globals: 3 registres trobats en 0.02 segons.
Articles, 3 registres trobats
Articles 3 registres trobats  
1.
25 p, 7.3 MB Geometry and kinematics of the Baza Fault (central Betic Cordillera, South Spain) : insights into its seismic potential / Medina-Cascales, Iván (Universitat d'Alacant. Departament de Ciències de la Terra i del Medi Ambient) ; Martin-Rojas, Iván (Universitat d'Alacant. Departament de Ciències de la Terra i del Medi Ambient) ; García-Tortosa, Francisco Juan (Universidad de Jaén. Departamento de Geología) ; Peláez Montilla, José A. (Universidad de Jaén. Departamento de Física) ; Alfaro García, Pedro (Universitat d'Alacant. Departament de Ciències de la Terra i del Medi Ambient)
The geometry and kinematics of active faults have a significant impact on their seismic potential. In this work, a structural characterization of the active Baza Fault (central Betic Cordillera, southern Spain) combining surface and subsurface data is presented. [...]
2020 - 10.1344/GeologicaActa2020.18.11
Geologica acta, Vol. 18 (2020) , p. 1-25 (Articles)  
Registre complet - Creative Commons
2.
21 p, 2.5 MB Paleoseismic analysis of the San Vicente segment of the El Salvador Fault Zone, El Salvador, Central America / Canora, Carolina (Universidad Complutense de Madrid. Departamento de Geodinámica, Estratigrafía y Paleontología) ; Villamor, P. (GNS Science) ; Martínez Día, J. J. (Universidad Complutense de Madrid. Departamento de Geodinámica, Estratigrafía y Paleontología) ; Berryman, K. R. (GNS Science) ; Álvarez Gómez, José A. (Universidad de Cantabria. Instituto de Hidráulica Ambiental) ; Capote, Ramón (Universidad Complutense de Madrid. Departamento de Geodinámica, Estratigrafía y Paleontología) ; Hernández, W. (Servicio Nacional de Estudios Territoriales (El Salvador))
The El Salvador earthquake of February 13th 2001 (Mw 6. 6) was associated with the tectonic rupture of the El Salvador Fault Zone. Paleoseismic studies of the El Salvador Fault Zone undertaken after this earthquake provide a basis for examining the longer history of surface rupturing earthquakes on the fault. [...]
2012 - 10.1344/105.000001700
Geologica acta, Vol. 10, Núm. 2 (June 2012) , p. 103-123  
Registre complet - Creative Commons
3.
12 p, 979.6 KB The active fault belts in eastern Tibet margin inferred using magnetotellurics / Zhao, G. (Institute of Geology, China Earthquake Administration) ; Wang, L. (Institute of Geology, China Earthquake Administration) ; Chen, X. (Institute of Geology, China Earthquake Administration) ; Tang, J. (Institute of Geology, China Earthquake Administration) ; Wan, Z. (Institute of Geology, China Earthquake Administration) ; Zhan, Y. (Institute of Geology, China Earthquake Administration) ; Xiao, Q. (Institute of Geology, China Earthquake Administration) ; Cai, J. (Institute of Geology, China Earthquake Administration) ; Zhang, J. (Earthquake Administration of Shandong Province) ; Wang, J. (Institute of Geology, China Earthquake Administration)
A magnetotelluric (MT) sounding has been carried out in the eastern margin of the Tibetan plateau. The survey line is about 145 km long, trending in NEE direction and crossing the Daliangshan block in the eastern edge of the Tibetan plateau. [...]
2010 - 10.1344/105.000001518
Geologica acta, Vol. 8, Núm. 1 (Març 2010) , p. 99-110  
Registre complet - Creative Commons

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