Evolución del paisaje en la cuenca baja del río Jarama [PDF]
This work aims to describe and to analyse natural and anthropic landscape in south-east of Madrid during the last fourteen years. The area is located on lower Jarama’s basin, inside the Comunity of Madrid, and is characterized by its little lanscape ...
García Rodríguez, M.ª del Pilar +1 more
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Interpretación del mapa de Anomalías de Bouguer de la zona nororiental de la Cuenca de Madrid
, 1993 The gravity field in the Ne zone of the Madrid Basin and conterminous areas is characterised by a number of regionally important anomalies referred to gradients and minimum and maximum axes. The Ledanca gradient separates two domains. Northwest of it, the hercynian basement structures are overprinted by the southern Central Systemalpine thrusts, which ...
Bergamín, J. F. +2 more
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Consumer populations and nutritional transition in Spain in the 20th century: A methodology for their reconstruction [PDF]
One feature of the modern nutrition transition is the growing consumption of animal proteins. The most common approach in the quantitative analysis of this change used to be the study of averages of food consumption. But this kind of analysis seems to be
Francisco Muñoz-Pradas
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La evolución geomorfológica de la cuenca de drenaje del río Lozoya (Comunidad de Madrid, España) [PDF]
, 2015 La presente Tesis Doctoral se planteó para analizar la evolución del paisaje de la cuenca del Río Lozoya, motivada por las características geomorfológicas singulares que presenta al tratarse de una cuenca intramontana desarrollada íntegramente dentro del Sistema Central.
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Análisis tensorial de la deformación superpuesta en el límite oriental de la cuenca de Madrid
, 1994 An analysis of Neogene brittle deformation using fault population analysis methods has been carried out between the SW border of the Iberian Range and Altomira Range. Two main paleostress fields have been established: 1) N70E - N120E compression (Altomira paleostress field) ofLate Oligocene - Early Miocene age that induced the formation of the SW ...
Muñoz Martín, Alfonso +2 more
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, 2008 At present, the water resources are a strategic element each time more necessary and limited becoming a source of conflicts. For that, it is fundamental to create an independent and competent entity with good reputation and social acceptation.
Andina de la Fuente, Diego +3 more
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Tipología y significado de bioturbaciones en facies evaporíticas continentales: Mioceno de la Cuenca de Madrid [PDF]
, 1997 Los complejos lacustres desarrollados durante el Mioceno en la Cuenca de Madrid están en buena parte constituidos por depósitos evaporíticos dentro de los cuales se reconocen diversos tipos de icnitas. En función del grado de bioturbación del sedimento, de la geometría y morfología de las trazas, sus dimensiones, estructuración interna y tipo de ...
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Significado de bioturbaciones en un medio evaporítico continental (Mioceno de la Cuenca de Madrid)
, 1992 Several types of bioturbation traces have been recognized within sedimentary deposits belonging to the Miocene Lower and Intermediate Units of the Eastern part of the Madrid Basin. The bioturbation traces are developed in muddy, carbonate and gypsiferous deposits that are interpreted as mudflat, ephemeral ponds and brackishto-saline lake facies.
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Correction: Validity and reliability of an protocol of the stomatognathic and postural system evaluation for patients with obstructive sleep apnea: a cross-sectional study. [PDF]
Front PhysiolGuijarro-Herraiz M +4 more
europepmc +1 more source
, 1999 The topmost alluvial deposits that outcrop adjacent to Central System igneous rocks are arranged in two units with particular internal architecture. The lower unit consists of ten bodies laterally disposed and bounded by concave erosiona! surfaces.
Santisteban, Juan Ignacio +3 more
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