A5018891388- Geological and Geophysical Studies Worldwide
- earthquake and tectonic studies
- Geological and Geochemical Analysis
- Geology and Paleoclimatology Research
- Geological formations and processes
- Landslides and related hazards
- Geological and Tectonic Studies in Latin America
- Karst Systems and Hydrogeology
- Comparative constitutional jurisprudence studies
- Archaeological and Historical Studies
- Legal processes and jurisprudence
- Archaeological and Geological Studies
- Comparative International Legal Studies
- Medieval Architecture and Archaeology
- Geophysical Methods and Applications
- Rock Mechanics and Modeling
- Neuroscience and Neural Engineering
- Geotourism and Geoheritage Conservation
- Seismic Waves and Analysis
- Seismic Imaging and Inversion Techniques
- Aeolian processes and effects
- 3D Surveying and Cultural Heritage
- Ethics and bioethics in healthcare
- Libraries, Manuscripts, and Books
- Tree-ring climate responses
Universidad de Zaragoza
2015-2024
National Research Council
2010
Universidad Complutense de Madrid
2010
University of Buenos Aires
1989
University of Utah
1984-1986
The relative position of our skeletal body parts is determined by the angles joints. In absence visual cues, joint angle information becomes conscious through a mental image (body image). Introspective attention to indicates that we have following sensory concerning particular joint: knowledge 1. both when moving and stationary, an awareness 2. direc tion 3. speed angular changes. These three types can vary independently (e.g. given be reached movements
A general synthesis of the recent and present stress situation evolution in Iberian Peninsula was obtained from microstructural seismological analysis. The deduced (1) fault population analysis (FPA) 409 sites distributed throughout Peninsula, (2) paleostress indicators given by 324 stations taken bibliography, (3) seismic data corresponding to 161 focal mechanisms evenly spread studied region. application FPA together with determination tensors for whole microplate has provided two main...
Among the conspicuous extensional structures that accommodate onshore deformation of Valencia Trough at centraleastern Iberian Chain, a number large faults show evidence activity during Pleistocene times. At eastern boundary Jiloca graben, Concud fault has moved since mid Pliocene times an average rate 0.07-0.08 mm/y, while rates from 0.08 to 0.33 mm/y have been calculated using distinct stratigraphic markers Middle Late age. A total nine paleoseisms associated this identified between 74.5...
By means of fault population analysis (using the right dihedra, y‐R diagram and Etchecopar's methods), states stress in a number sites Cameras Massif (Northwestern Iberian Chain, Spain) nearby areas Ebro Basin have been determined. These used as framework order to infer model actual field that area during main stage Alpine compression (Oligocene‐lower Miocene). The three directions obtained (NW‐SE, NNE, NE‐SW) can be explained by single with horizontal σ 1 trending NNE vertical 2 , whose...
The Jiloca basin is a large intramontane, NNW–SSE-trending topographical depression in which the relative role of tectonic subsidence and erosional lowering currently matter discussion. Geometry facies sedimentary infill at its central sector have now been characterized from compiled borehole data, allows discussions how evolutionary model constrained. contains Late Pliocene to Pleistocene sequence made up alluvial fan, pediment mantle episodic palustrine deposits, overlying carbonate unit...
Abstract A kinematical model for the Utrillas thrust is proposed, including reconstruction of incremental slip history, progressive internal deformation and tectono-sedimentary relationships at Montalbán (foreland) Aliaga (piggy-back) Tertiary basins. 3D geometrical main surface, defined by ramps oriented NE–SW, east–west, NW–SE north–south, reconstructed from cross-sections. Besides, sheet internally deformed two main, frequently superposed fold sets, trending to NNW–SSE (earlier) east–west...