A5056675877- Geology and Paleoclimatology Research
- Geological and Geophysical Studies Worldwide
- Geological formations and processes
- Evolution and Paleontology Studies
- earthquake and tectonic studies
- Geological and Geochemical Analysis
- Archaeological and Geological Studies
- Geomagnetism and Paleomagnetism Studies
- Paleontology and Stratigraphy of Fossils
- Pleistocene-Era Hominins and Archaeology
- Geological Modeling and Analysis
- Botany and Plant Ecology Studies
- Bioenergy crop production and management
- Mycorrhizal Fungi and Plant Interactions
- Geological Formations and Processes Exploration
- Plant Diversity and Evolution
- Forest Biomass Utilization and Management
- Mediterranean and Iberian flora and fauna
- Seismic Imaging and Inversion Techniques
- Masonry and Concrete Structural Analysis
- Archaeological and Historical Studies
- Atmospheric and Environmental Gas Dynamics
- Physical Education and Sports Studies
- 3D Surveying and Cultural Heritage
- Ancient and Medieval Archaeology Studies
Universitat de Barcelona
2009-2018
Repsol (Spain)
2018
University of Parma
1985-2007
ABSTRACT This paper presents new magnetostratigraphic results from a 1100‐m‐thick composite section across the marine to continental sediments of central part SE margin Ebro basin (NE Spain). Integration with existing and biochronological data allows robust correlation geomagnetic polarity time scale. The resulting absolute chronology ranges 36.3 31.1 Ma (Priabonian Rupelian), yields an interpolated age ∼36.0 (within chron C16n.2n) for youngest eastern basin. is in concordance...
Long-period orbital forcing is a crucial component of the major global climate shifts during Cenozoic as revealed in marine pelagic records. A complementary regional perspective change can be assessed from internally drained lake basins, which are directly affected by insolation and precipitation balance. The Ebro Basin northeastern Iberia embraces 20 Myr long continuous sedimentary record where recurrent expansions retractions central lacustrine system suggest periodic water balance due to...
This study presents a combined biostratigraphic (calcareous nannofossils, larger foraminifers) and magnetostratigraphic of the Middle Late Eocene marine units Igualada area, eastern Ebro Basin. The studied sections Santa Maria de Miralles La Tossa encompass complete succession Group, where assemblages rich in foraminifers have been since early 1950's. A total 224 paleomagnetic sites 62 samples were collected along 1350m-thick section that ranges from chron C20n to C16n (~43Ma ~36Ma)....
The precise determination of the tectonic deformation timing such as thrust emplacement has always been a challenge for understanding evolution fold-and-thrust belts. In Catalan Coastal Ranges, this issue traditionally addressed through mapping and analysis syn-tectonic successions preserved in SE margin Ebro Basin. However, age Paleogene contractional structures located towards hinterland responsible inversion uplift inherited Mesozoic structure remained uncertain due to lack syn-kinematic...
Paleoclimatic reconstructions of the Eocene-Oligocene transition indicate significant spatial heterogeneity in both marine and terrestrial responses to formation ice sheets on Antarctica. Marine isotopic records that cooling volume effects contributed a shift approximately +1.1‰ benthic planktonic foraminiferal δ18O. Because generally are lower temporal resolution, deconvolving temperature from has been more challenging. New results based paleosols well-dated sequence Ebro Basin (Spain)...
Abstract A magnetostratigraphy‐based chronological framework has been constructed in the E ocene sediments of M ontserrat alluvial fan/fan‐delta complex (southeast bro B asin), order to unravel forcing controls on their sequential arrangement and revise tectonosedimentary history region. The palaeomagnetic study is based 403 sites distributed along an 1880‐m‐thick composite section, provides improved temporal constraints independent correlation geomagnetic polarity time scale. new together...
A charophyte biozonation for the transitional and continental Upper Eocene-Lower Oligocene record in eastern margin of Ebro Basin is performed calibrated using magnetostratigraphic data. This study has been based on intensive sampling collected along five composite sections. The Harrisichara vasiformis-tuberculata European biozone renamed to H. lineata biozone, since former index-species was a poorly characterised morphotype with non-valid species name. represented Sant Boi Formation...
Research Article| July 01, 2004 Modeling deformation and salt tectonics in the eastern Mediterranean Ridge accretionary wedge E. Costa; Costa 1Dipartimento di Scienze della Terra, Parco Area delle 157/A, 43100 Parma, Italy Search for other works by this author on: GSW Google Scholar A. Camerlenghi; Camerlenghi 2Istituto Nazionale Oceanografia e Geofisica Sperimentale—OGS, Borgo Grotta Gigante 42/c, I-34010 Sgonico (TS), Polonia; Polonia 3Istituto Geologia Marina, CNR, Via Gobetti 101, 40129,...
Abstract The Neogene Crotone basin in eastern Calabria contains extensive Messinian evaporite deposits, including thick gypsarenite and halite. halite deposit reaches a maximum thickness of c . 300 m some areas forms relatively small diapirs piercing late Pliocene sediments. Halite is strongly modified by folding recrystallization, but few primary features are preserved. Four facies have been recognized: (a) banded consisting folded white dark bands deposited salt pan and/or saline mudflat;...
New Magnetostratigraphic data from the Montserrat alluvial fan and fan-delta system led to an unambiguous correlation GPTS provided basis for a quantitative estimate of its tectonosedimentary evolution. Local isostatic backstripping analysis has been performed. Tectonic pulses in basin margin during initial synsedimentary folding episode, expressed by unconformities forelimb rotation rates, correlate tectonic subsidence which shows trend similar rates. Three different frequency scales...
<p>Carbonated rocks are crucial targets for oil exploration, outcropping often in large areas with minimum spectral differences among geological units. The typical carbonate absorptions 2200 nm and 2300 nm, excluded from the wavelength range of AISA Eagle II. II hyperspectral data processed flight lines 1024 swath pixels visible to near-infrared (400 970 nm). has a spatial resolution 1 m records total 128 channels 4,8 nm. area study is rocky mountain densely vegetated, covered by...