Welcome to my webpage !
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To answer these questions, I use a multidisciplinary and multiple-timescale toolkit:
- Tectonic Geomorphology:
quantitative geomorphic analysis of deformed Quaternary deposits to determine fault kinematics and constrain long-term
(1-100 ka) tectonic offsets,
- Paleo-seismology:
excavation of trenches across active faults to unravel the paleo-earthquakes history (1-10 ka),
- Geodesy:
monitoring of present-day crustal deformation (GPS) (1-10 years),
- Structural Geology:
drawing relationships between active deformation and geological structures, use of subsurface geometry of thrust faults
and deformation models to convert surface uplift or folding into cumulative slip on the fault plane,
- Quaternary Geochronology:
dating of cumulative strain markers, typically Quaternary alluvial deposits (luminescence dating, cosmogenic exposure
dating, 14C).
I am also interested in what related archives from archaeology, paleo-climates, pedology, river processes... can bring
to bear on the above questions.
- Tectonic Geomorphology:
quantitative geomorphic analysis of deformed Quaternary deposits to determine fault kinematics and constrain long-term
(1-100 ka) tectonic offsets,
- Paleo-seismology:
excavation of trenches across active faults to unravel the paleo-earthquakes history (1-10 ka),
- Geodesy:
monitoring of present-day crustal deformation (GPS) (1-10 years),
- Structural Geology:
drawing relationships between active deformation and geological structures, use of subsurface geometry of thrust faults
and deformation models to convert surface uplift or folding into cumulative slip on the fault plane,
- Quaternary Geochronology:
dating of cumulative strain markers, typically Quaternary alluvial deposits (luminescence dating, cosmogenic exposure
dating, 14C).
I am also interested in what related archives from archaeology, paleo-climates, pedology, river processes... can bring
to bear on the above questions.