| Registros del 1 al 10 de 15 encontrados |
1.- Active faults and folds in the southeastern boundary of the Betic Cordilleras
[International Geological Congress]; [location varies]; III; International, 2004
Italia 2004; 32nd international geological congress; abstracts
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2.- ACTIVE FAULTS, SEISMICITY AND STRESSES IN AN INTERNAL BOUNDARY OF A TECTONIC ARC; CAMPO DE DALIAS AND NIJAR, SOUTHEASTERN BETIC CORDILLERAS, SPAIN
ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 2005
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3.- Changing tectonic styles of recent and active structures in the Rif Cordillera and asymmetry in respect to the Betic Cordillera (western Mediterranean)
[International Geological Congress]; [location varies]; III; International, 2008
33rd international geological congress; abstracts
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4.- Crustal-scale transcurrent fault development in a weak-layered crust from an integrated geophysical research; Carboneras fault zone, eastern Betic Cordillera, Spain
American Geophysical Union and The Geochemical Society;; USA; United States, 2010
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5.- Deep deformation pattern from electrical anisotropy in an arched orogen (Betic Cordillera, western Mediterranean)
Geological Society of America (GSA); Boulder, CO; USA; United States, 2010
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6.- Deep structure of a mountain front with olistostrome development from gravity, MT and seismicity data (Guadalquivir Basin, central Betic Cordilleras)
[International Geological Congress]; [location varies]; III; International, 2008
33rd international geological congress; abstracts
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7.- Deformation behaviour of the low-rate active Balanegra fault zone from high-precision levelling (Betic Cordillera, SE Spain)
Elsevier; Oxford; GBR; United Kingdom, 2013
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8.- Fault and fold interaction during the development of the Neogene-Quaternary Almeria-Nijar Basin (SE Betic Cordilleras)
Geological Society of London; London; GBR; United Kingdom, 2006
Tectonics of the western Mediterranean and North Africa
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9.- FAULTED HYBRID JOINTS; AN EXAMPLE FROM THE CAMPO DE DALIAS (BETIC CORDILLERAS, SPAIN)
ELSEVIER; OXFORD; III; INTERNATIONAL, 2004
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10.- Folds evolution and basin development in the hinterland of an orogen; the Almanzora Neogene-Quaternary Corridor (SE Betic Cordillera, Spain)
IUGG; [location varies]; III; International, 2007
Earth; our changing planet; proceedings of IUGG XXIV general assembly
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