A5053923803- Geological and Geophysical Studies Worldwide
- Geology and Paleoclimatology Research
- Geological formations and processes
- Archaeological and Geological Studies
- Geological and Tectonic Studies in Latin America
- earthquake and tectonic studies
- Geological and Geochemical Analysis
- Archaeological and Historical Studies
- Paleontology and Stratigraphy of Fossils
- Evolution and Paleontology Studies
- Historical and socio-economic studies of Spain and related regions
- Landslides and related hazards
- Geological and Geophysical Studies
- Karst Systems and Hydrogeology
- Paleontology and Evolutionary Biology
- Hydrocarbon exploration and reservoir analysis
- Medieval Architecture and Archaeology
- Mediterranean and Iberian flora and fauna
- Aeolian processes and effects
- Geophysical Methods and Applications
- Seismic Imaging and Inversion Techniques
- Geomagnetism and Paleomagnetism Studies
- Methane Hydrates and Related Phenomena
- Environmental and Ecological Studies
- High-pressure geophysics and materials
Universidad de Zaragoza
2015-2024
International Union of Railways
2017
Cardiff University
2003
In the Galve sub-basin, sedimentary record of Upper Hauterivian–Lower Barremian El Castellar Formation is divided into two stages by a marlstone interval with gypsum. Stage 1 shows great variety subenvironments and facies (alluvial, palustrine lacustrine) whereas in stage 2 an extensive, shallow carbonate lake developed. Sedimentation was controlled system south-dipping, ENE–WSW listric normal faults, laterally bounded NNW–SSE steeper transfer faults. Faults sedimentation from basin scale...
Abstract An aeolian dune field migrating to the east encroached on toes of alluvial fans in Teruel Basin (eastern Spain) during a short interval Late Pliocene ( ca 2·9 2·6 Ma), when Northern Hemisphere glaciation and strong glacial–interglacial cycles began. Preservation was controlled by syn‐sedimentary activity normal fault. Ephemeral water discharge eroded sands formed V‐shaped channels which sandstone blocks accumulated. The incorporation loose sand wadi waters modified sediment/water...
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...
Research Article| March 01, 2001 Slumping and a sandbar deposit at the Cretaceous-Tertiary boundary in El Tecolote section (northeastern Mexico): An impact-induced sediment gravity flow Ana R. Soria; Soria 1Departamento de Ciencias la Tierra, Universidad Zaragoza, E-50009, Spain Search for other works by this author on: GSW Google Scholar Carlos L. Liesa; Liesa Maria Pilar Mata; Mata 2Facultad del Mar, Departamento Geología, Cádiz, Puerto Real, E-11510, José A. Arz; Arz 3Facultad Autónoma...
Terra Nova, 23, 76–84, 2011 Abstract The Triassic Buntsandstein facies in the north‐eastern Iberian Chain (central eastern Spain), previously considered to be fluvial origin, is shown contain an evolving erg system. preserved accumulation comprises a succession that represents transition from wadi belt via inner erg‐margin central‐erg This study supports Early (Olenekian) palaeoclimate models for Western Europe, which predict (extremely) arid conditions Iberia. two main easterly and...
ABSTRACT In the El Mulato section (NE Mexico), Upper Cretaceous marly Méndez and Lower Palaeogene Velasco Formations are separated by a clastic unit. Benthic foraminifera from both formations indicate lower bathyal depths. The unit, in contrast, contains platform sands, muddy pebbles neritic (shallow) faunas mixed with microspherules, indicating that it was allochthonously deposited into deep basin. diversity variability origin of components its sedimentological features, support model...