Zobrazeno 1 - 6
of 6
pro vyhledávání: '"J. J. Martínez-Diaz"'
Autor:
E. Gràcia, R. Bartolome, C. Lo Iacono, X. Moreno, D. Stich, J. J. Martínez-Diaz, G. Bozzano, S. Martínez-Loriente, H. Perea, S. Diez, E. Masana, J. J. Dañobeitia, O. Tello, J. L. Sanz, E. Carreño, EVENT-SHELF Team
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 12, Iss 11, Pp 3255-3267 (2012)
Recently acquired swath-bathymetry data and high-resolution seismic reflection profiles offshore Adra (Almería, Spain) reveal the surficial expression of a NW–SE trending 20 km-long fault, which we termed the Adra Fault. Seismic imaging across the
Externí odkaz:
https://doaj.org/article/44798cbd2d8d4002ad97e4cc1e3b2abe
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 23, Pp 2031-2052 (2023)
Strike-slip fault ruptures have a limited capacity to generate vertical deformation, and for this reason they are usually dismissed as potential destructive tsunami sources. At the western tip of the western Mediterranean, in the Alboran Sea, tectoni
Externí odkaz:
https://doaj.org/article/dbf5a66f72c548b28561442d57a5cc71
Autor:
J. García-Mayordomo, R. Martín-Banda, J. M. Insua-Arévalo, J. A. Álvarez-Gómez, J. J. Martínez-Díaz, J. Cabral
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 17, Pp 1447-1459 (2017)
Active fault databases are a very powerful and useful tool in seismic hazard assessment, particularly when singular faults are considered seismogenic sources. Active fault databases are also a very relevant source of information for earth scientis
Externí odkaz:
https://doaj.org/article/b9629e746f9d42cbbf7d7a787c950806
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 16, Pp 2273-2286 (2016)
Transition from endorheic alluvial fan environments to well-channelized fluvial systems in natural conditions may occur in response to base-level fluctuations. However, human-induced changes in semi-arid regions can also be responsible for similar
Externí odkaz:
https://doaj.org/article/dc9e5e22578e4b43aa9e27fc11df2eca
Autor:
J. J. Martínez-Díaz
Publikováno v:
Estudios Geologicos, Vol 55, Iss 5-6, Pp 251-266 (1999)
En este trabajo se presenta el estudio sismotectónico de la falla oblicua (inversodireccional) de Alhama de Murcia y su entorno. Se analiza la distribución espacial y temporal de la sismicidad histórica e instrumental en el entorno de la falla y s
Externí odkaz:
https://doaj.org/article/67b5775978664c62a5c3ef88832dfd10
Publikováno v:
Annals of Geophysics, Vol 46, Iss 5 (2003)
In this work we present a study of an alluvial fan system, which is affected by the Quaternary activity of the leftlateral, reverse Alhama de Murcia Fault (Betic Cordillera). Paleoseismic studies in this area yield data that can be compared and cor
Externí odkaz:
https://doaj.org/article/f1d58f6c9fec472a9235e1faa24696b0