Nicolas Loget

Maitre de conférences, Université Pierre et Marie Curie

75005ParisÎle-de-France - France

Geologist, expertise in Basin analysis/quantitative geomorphology
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Basin analysis :
-Sequential stratigraphy (basin and incised valleys)
-Mass balance (erosion/sedimentation)
-Tectonic and sismotectonic analysis


Quantitative geomorphology :
-Dynamics of river processes
-Incision of rivers linked to base-level fall (quaternary, messinian)
-Comparison earth drainage network/mars drainage network



Publications
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-Michard A., Dumont T., Andréani L., and Loget N.(accepté), Synsedimentary detachment on a former passive margin : the ante-Senonian Dévoluy unconformity revisited (Southern Subalpine Chains, France) Volume special BSGF Provence.
-Loget N. and Van Den Driessche J., (2009), Wave train model for knickpoint migration. Geomorphology, 106, 376–382.
-Loget N., Davy P., and Van den Driessche J., (2006), Mesoscale fluvial erosion parameters deduced from the modeling of the Mediterranean sea-level drop during the Messinian (Late Miocene). Journal of Geophysical Research, 111, F03005, doi:10.1029/2005JF000387.
-Loget N. and Van Den Driessche J., (2006), On the origin of the Strait of Gibraltar. Sedimentary geology, 188-189, 341–356.
-Babault J., Loget N., Castelltort, S., Van Den Driessche, J., Bonnet, S. and Davy P., (2006) Did the Ebro connect to the Mediterranean before the Messinian salinity crisis ? Geomorphology, 81, 155–165.
-Loget N., Van den Driessche J., and Davy P., (2005), How did the Messinian Salinity Crisis end ? Terra Nova, 17, 414–419.


Technical reports
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-Loget N. and Lericolais G. (2009), Catalog of physiographic and sedimentologic observations of shelfal to deepwater Quaternary systems, part2: the Black Sea, a semi-enclosed basin with fast transgression and climate driven system, Catalogue EXXONMOBIL/IFREMER, 17 p.
-Le Pichon X., Rangin C., Loget N., Hamon Y., Lin J.Y, Andréani L. (2008), Tectonique provençale et sismicité associée : rôle des phénomènes gravitaires et diapiriques. Rapport final programme CASHIMA/CEA Cadarache, 124 p.
-Loget N. (2005), Dynamique de l’érosion consécutive à une chute du niveau de base. L’exemple de la Crise de Salinité Messinienne. Mémoires de Géosciences Rennes, vol. 119, 226 p.

Nicolas Loget
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