Browsing by Subject "Folds"
Now showing items 1-9 of 9
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Deformaciones tectónicas desde el Tortoniense en el Campo de Dalias (Cordilleras Béticas)
(Sociedad Geológica de España, 2002)The Campo de Dalias is an emerged zone located at the northern boundary of Alboran Sea. The Neogene-Quaternary sediments of the Campo de Daifas are deformed by E-W open folds that also uplift Sierra de Cádor. The field ... -
Estiramiento paralelo a los ejes de los pliegues en la Unidad de las Nieves (Dominio de Alborán, Béticas Occidentales)
(Sociedad Geológica de España, 2020)El estiramiento paralelo a las directrices estructurales es un mecanismo fundamental en la cinemática de los arcos orogénicos. Se analiza el caso de las Unidades Frontales -parte más externa de las Zonas Internas- de la ... -
«La Falla de Urriza (Pirineo Occidental): Neotectónica en materiales del cretácico superior del norte de Navarra»
(Sociedad Geológica de España, 1990)In the north of Navarra (Western Pyrenees), subvertical folds with characteristic density of diaclases in the hinge zone outcrop in upper cretaceous beds. Its genesis has been associated to a sinistral wrench affecting ... -
Geometría de los volcanes de lodo y de los pliegues de la Dorsal Mediterránea al Sur de Creta (Mediterráneo Oriental)
(Sociedad Geológica de España, 1994)Side scan sonar images and high resolution profiles obtained with the R/V Gelendzhik in the 1993 cruise of the TREDMAR program, give new information on the geometry of the mud volcanoes, folds and fractures located in the ... -
Medida de la deformación de pliegues en el extremo oriental del Sistema Central español
(Sociedad Geológica de España, 1987)We propose an areal distribution for the second phase hercynian folds in the eastermost part of the Spanish Central System, based on their morphological charactheristics. The analysis of these data allows us to calculate ... -
Nuevos datos sobre la fase de deformación sárdica. Geometría de los pliegues pre-hercínicos del río Salor (Cáceres)
(Sociedad Geológica de España, 1986)A study made over some 50 pre-hercinian folds shows how the attitude of their axes are in the NE-SW quadrants, being similar to the attitude of those of the Sardic fase known up to now in the Zona Centroibérica. The exam ... -
Orientaciones de las estructuras de plegamiento en un sector de la Cordillera Ibérica
(Sociedad Geológica de España, 1987)In the area dealt with here, the large folds show different directions that may be grouped into two main sets: the most important correspond to the called "Iberian directions», around 130º E, and the second to the «Guadarrama ... -
Pliegues eocenos de dirección N-S en el Pirineo occidental
(Sociedad Española de Geología, 2001)Several N-S trending folds have been identified in the Eocene strata of the western Pyrenees. Stratigraphical and sedimentological lines of evidence show that they formed from late Ypresian to middle Lutetian times. These ... -
Pliegues limitados por fallas en el subbético medio (sector de torre cardela, Granada)
(Sociedad Geológica de España, 2003)In the area of Torre Cardela, situated to the NE of Granada, there are NE-SW to NNE-SSW folds comprised among ENE-WSW dextral strike-slip fauts. The formation of all these structures are interpreted as singenetic, within ...