A5043355466- Geological and Geochemical Analysis
- Geological and Geophysical Studies Worldwide
- earthquake and tectonic studies
- Geological formations and processes
- Geology and Paleoclimatology Research
- Geological Studies and Exploration
- Radiomics and Machine Learning in Medical Imaging
- Geochemistry and Geologic Mapping
- Lipid Membrane Structure and Behavior
- Orthopedic Surgery and Rehabilitation
- Nanopore and Nanochannel Transport Studies
- Spectroscopy and Quantum Chemical Studies
- Dental Implant Techniques and Outcomes
- High-pressure geophysics and materials
- Geomagnetism and Paleomagnetism Studies
- Dental materials and restorations
Sorbonne Université
2022-2023
Institut des Sciences de la Terre de Paris
2022-2023
Centre National de la Recherche Scientifique
2022-2023
University of Tennessee at Knoxville
2020
Baylor College of Medicine
2003
University of Toronto
2003
Understanding the evolution of convergent plate boundaries and mechanisms strain accommodation through time space is made possible by studying exhumed subduction complexes within orogenic belts. This study uses internal zones Western Alps, one largest best-preserved fossil in world, to track transition from collision. We herein combine in-situ Ar-Ar Rb-Sr data on white micas with pressure-temperature estimates derived pseudosection modeling Raman thermometry carbonaceous material, along...
Abstract In the Western Alps, oceanic lithosphere fragments recovered from subduction are exposed continuously across Liguro‐Piemont domain. this nappe‐stack, Schistes Lustrés metasediments volumetrically dominant and contain large amounts of high‐pressure lawsonite‐ Fe‐Mg carpholite‐bearing veins. These veins formed close to peak burial conditions at 30–60 km depth where deep slow slips tremors occur. 12 studied outcrops, vein thickness distribution fit power laws while spacings clustering...
Abstract Continental subduction and collision are not merely follow-ups of oceanic but mark the transition from lithospheric-scale deformation localized along interface to crustal-scale distributed across orogen. In order unravel processes typifying dynamic changes collision, we have characterized pressure-temperature (P-T) spatio-temporal evolution rocks on each side tectonic contact (Briançonnais–Liguro-Piemont [Br-LP] contact) separating subducted remnants continental fragments Western...
Continental subduction and collision are not merely follow-ups of oceanic but mark the transition from lithospheric-scale deformation localized along interface to crustal-scale distributed across orogen. In order unravel processes typifying dynamic changes collision, we have characterized pressure-temperature (P-T) spatio-temporal evolution rocks on either side tectonic contact (Briançonnais/Liguro-Piemont – Br/LP contact) separating subducted remnants continental...
<p>Detailed methodology of peak pressure and temperature estimations, location samples detailed results conditions. </p>
<p>Detailed methodology of peak pressure and temperature estimations, location samples detailed results conditions. </p>
&lt;p&gt;Fragments of subducted slow-spreading oceanic lithosphere are exposed continuously in the Liguro-Piemont domain Western Alps. By combining new and literature petrological data, interpolated maps maximum temperatures, Si contents phengite as a proxy for peak pressure thermodynamic modelling, we provide detailed framework metamorphic conditions experienced by distinct subduction slices. High-resolution mapping confirms marked eastward increase grade throughout domain, well...