A5068542990- Geological and Geophysical Studies Worldwide
- Archaeological and Historical Studies
- Archaeological and Geological Studies
- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Geology and Paleoclimatology Research
- Geological formations and processes
- Soil erosion and sediment transport
- Environmental and Ecological Studies
- Geophysical and Geoelectrical Methods
- Heavy metals in environment
- Karst Systems and Hydrogeology
- Landslides and related hazards
- Geochemistry and Geologic Mapping
- Groundwater and Isotope Geochemistry
- Geophysics and Gravity Measurements
- Rock Mechanics and Modeling
- Geological Formations and Processes Exploration
- Fluoride Effects and Removal
- Geological Modeling and Analysis
- Seismic Waves and Analysis
- Geophysical Methods and Applications
- Geotechnical Engineering and Analysis
- Geomagnetism and Paleomagnetism Studies
Institut Cartogràfic i Geològic de Catalunya
1995-2022
Universitat de Barcelona
1986-1995
Research Article| May 01, 2016 Provenance, age, and tectonic evolution of Variscan flysch, southeastern France northeastern Spain, based on zircon geochronology F.J. Martínez; Martínez 1Departament de Geologia, Universitat Autònoma Barcelona, 08193 Bellaterra, Spain Search for other works by this author on: GSW Google Scholar C. Dietsch; Dietsch † 2Department Geology, University Cincinnati, Ohio 45221-0013, USA †dietscc@ucmail.uc.edu J. Aleinikoff; Aleinikoff 3U.S. Geological Survey, MS 963,...
ABSTRACT Mapping bedrock structure beneath overburden is crucial for understanding geological and hydrogeological processes. Acquiring this information generally done using well drilling or geophysical surveys; but these studies are expensive require large periods of acquisition processing time. In addition, data can be logistically challenging in urban zones with limited available areas instrumentation deployment. Under favourable conditions (1D high acoustic impedance contrast) the H/V...
<p>The Garraf Massif is a remarkable example of geodiversity in karstic environment. It located next to the Catalan coast, SW Barcelona city, and formed mainly by Cretaceous Jurassic carbonate rocks which karst develops. contains many exokarstic morphologies (microforms megaforms), as well an extraordinary endokarst, represented large caves deep vertical shafts, condition drainage.</p><p>Within framework "Geoanthropic Map Catalonia"...
<p>In the Central Pyrenees, where density contrast between Paleozoic rocks and intruded granitic bodies is measurable, geological cross-sections constrained with gravity data help to unravel subsurface geometry of granites.</p><p>With this goal in mind, during 2018 2019 several gravimetric surveys were carried out Pyrenees improve existent spatial resolution from databases Spanish Catalan Geological Surveys, especially La Maladeta Andorra Mont-Louis...
<p>The Lleida-Monzón Plain, with an area of 7.700 km<sup>2</sup>, is the largest transfer and storage zone in central-eastern South Pyrenees source outlet. It drains four main South-Pyrenean rivers: Cinca River, Noguera Ribagorçana Segre River joined to Pallaresa River. The covers about 13.600 km<sup>2</sup> forming part Pre-Pyrenees Pyrenees.</p><p>In we differentiate...
A well constrained crustal-scale balanced and restored cross - section through the Eastern Pyrenees provides basis for a multi-step flexural modelling of northeastern Iberian lithosphere during Eocene -Oligocene thrusting. The extends from Aquitanian Basin in North to Ebro València Trough South. Crustal parameters are by deep reflection profiles (ECORS VALSIS), refraction profiles, gravimetry magnetotellurics. Tectono -sedimentary relationships provide good time control both basement cover...