Zobrazeno 1 - 10
of 13
pro vyhledávání: '"José Jesús Martínez-Díaz"'
Autor:
Handoyo Handoyo, Irene DeFelipe, Raquel Martín-Banda, Julián García-Mayordomo, David Martí, José Jesús Martínez-Díaz, Juan Miguel Insua-Arévalo, Teresa Teixidó, Juan Alcalde, Imma Palomeras, Ramon Carbonell
Publikováno v:
Geologica Acta, Vol 20, Iss 9, Pp 1-19 (2022)
The seismicity in the SE Iberian Peninsula is distributed parallel to the coast in a well-developed strike-slip fracture system known as the Eastern Betic Shear Zone (EBSZ). This work focuses on the characterization of the shallow subsurface structur
Externí odkaz:
https://doaj.org/article/ad4e1cc6a73144fba6d8b81ef723d541
Autor:
Anna Martí, Pilar Queralt, Alex Marcuello, Juanjo Ledo, Emilio Rodríguez-Escudero, José Jesús Martínez-Díaz, Joan Campanyà, Naser Meqbel
Publikováno v:
Earth, Planets and Space, Vol 72, Iss 1, Pp 1-19 (2020)
Abstract The Lorca earthquake (May 11th, 2011, Mw 5.2) stands as the most destructive one in Spain over the last 50 years, interpreted as having occurred in an intersegment zone of the strike–slip Alhama de Murcia Fault (AMF) (Eastern Betics, Spain
Externí odkaz:
https://doaj.org/article/2d786874a4c94043b0c08ee398a986d1
Autor:
Jorge Alonso-Henar, Carlos Fernández, José Antonio Álvarez-Gómez, Carolina Canora, Alejandra Staller, Manuel Díaz, Walter Hernández, Ángela Valeria García, José Jesús Martínez-Díaz
Publikováno v:
Geosciences, Vol 12, Iss 7, p 266 (2022)
The El Salvador Fault Zone (ESFZ) is part of the Central American Volcanic Arc and accommodates the oblique separation movement between the forearc sliver and the Chortis block (Caribbean Plate). In this work, a triclinic transtension model was appli
Externí odkaz:
https://doaj.org/article/4af2defa930e4be08bd2d7cd5bbba438
SE Iberia is a tectonically active area with an important history of destructive earthquakes. Some of these earthquakes have been associated with known active faults, but the seismic source of most of them remains unclear. The majority of these earth
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::530e9574800afec38031c67f215ef509
https://doi.org/10.5194/egusphere-egu23-14995
https://doi.org/10.5194/egusphere-egu23-14995
Publikováno v:
Frontiers in Earth Science. 11
Continental carbonates, such as travertines and tufas, formed from CO2-rich groundwater degassing as it emerges at the Earth’s surface, are often associated with major crustal-scale faults. The Carraclaca site, in the Lorca-Totana section of the Al
Publikováno v:
SSRN Electronic Journal.
Autor:
Marta Béjar-Pizarro, Rosa María Mateos, Marco Luna, Kervin Chunga, Oriol Monserrat, José Antonio Álvarez Gómez, Aracely Lima, Jorge Pedro Galve, Gerardo Herrera, José Jesús Martínez Díaz, Alejandra Staller, Raúl Pérez-López
Publikováno v:
Remote Sensing
Volume 10
Issue 6
Pages: 899
E-Prints Complutense. Archivo Institucional de la UCM
instname
Digital.CSIC. Repositorio Institucional del CSIC
Digibug. Repositorio Institucional de la Universidad de Granada
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
Remote Sensing, Vol 10, Iss 6, p 899 (2018)
Volume 10
Issue 6
Pages: 899
E-Prints Complutense. Archivo Institucional de la UCM
instname
Digital.CSIC. Repositorio Institucional del CSIC
Digibug. Repositorio Institucional de la Universidad de Granada
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
Remote Sensing, Vol 10, Iss 6, p 899 (2018)
It has long been recognized that earthquakes change the stress in the upper crust around the fault rupture and can influence the behaviour of neighbouring faults and volcanoes. Rapid estimates of these stress changes can provide the authorities manag
Autor:
M. Blanco, José Jesús Martínez Díaz, Alberto Tomás Caselli, Pablo A. Euillades, Maria Laura Velez
Publikováno v:
Journal of Volcanology and Geothermal Research. 202:117-126
The Copahue volcano is one of the most active volcanoes in Argentina with eruptions having been reported as recently as 1992, 1995 and 2000. A deformation analysis using the Differential Synthetic Aperture Radar technique (DInSAR) was performed on Co
Autor:
Carolina Canora Catalán, María Pilar Villamor Pérez, José Jesús Martínez Díaz, Alejandra Staller, José Antonio Álvarez Gómez, Manuel Roberto Díaz Flores, Kelvin Berryman, Ramón Capote del Villar
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
[EN] The 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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7a98af04edc70aa3c40a318df9ceb87b
http://hdl.handle.net/10261/108297
http://hdl.handle.net/10261/108297
Autor:
Nemesio Heredia, Juan Miguel Insúa Arévalo, Alfonso Muñoz Martín, José Jesús Martínez Díaz, Antonio José Olaiz Campos, Gerardo de Vicente Muñoz, Fidel Martín-González, Loreto Antón
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM
The Northwest and Central-West Iberian Peninsula configure an intraplate area far from the active plate boundaries, where the Variscan basement crops out extensively (Iberian Massif). This area of the Iberian Peninsula has been traditionally consider
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1c1f9e48ad27fb061cbfd51537607e72
https://doi.org/10.5209/rev_JIGE.2012.v38.n1.39205
https://doi.org/10.5209/rev_JIGE.2012.v38.n1.39205