His primary areas of investigation include Geomorphology, Seismology, Thrust fault, Fluvial and Bedrock. His Geomorphology study integrates concerns from other disciplines, such as Crust and Décollement. When carried out as part of a general Seismology research project, his work on Terrane, Craton and Fault is frequently linked to work in Context, therefore connecting diverse disciplines of study.
As a part of the same scientific family, he mostly works in the field of Thrust fault, focusing on Erosion and tectonics and, on occasion, Late Miocene. His Fluvial research incorporates themes from Bed load, Pebble and Lithology. His work in Bedrock addresses subjects such as Denudation, which are connected to disciplines such as Structural basin, Drainage basin and Erosion.
Jérôme Lavé spends much of his time researching Geomorphology, Erosion, Denudation, Sediment and Paleontology. As part of one scientific family, he deals mainly with the area of Geomorphology, narrowing it down to issues related to the Crust, and often Lithosphere. In the subject of general Erosion, his work in Erodability is often linked to Cosmogenic nuclide, thereby combining diverse domains of study.
His Denudation study combines topics in areas such as Erosion and tectonics, Geochemistry, Plateau and Tectonic uplift. In his study, Seismology is strongly linked to Zircon, which falls under the umbrella field of Plateau. His Sediment research is multidisciplinary, incorporating elements of Hydrology, Floodplain, Structural basin and Weathering.
Jérôme Lavé mainly focuses on Erosion, Sediment, Denudation, Hydrology and Geochemistry. In his study, which falls under the umbrella issue of Erosion, Provenance and Suspended load is strongly linked to Drainage basin. His Sediment study is related to the wider topic of Geomorphology.
His Geomorphology research is multidisciplinary, relying on both Fault scarp and Mountain formation. The various areas that Jérôme Lavé examines in his Denudation study include Range, Quaternary, Foreland basin and Paleozoic. Jérôme Lavé has researched Hydrology in several fields, including Landslide, Sediment transport, Bedrock river and Clay minerals.
His scientific interests lie mostly in Geomorphology, Alluvium, Pleistocene, Sediment and Denudation. His study ties his expertise on Fold together with the subject of Geomorphology. The Alluvium study combines topics in areas such as Paleoseismology, Blind thrust earthquake, Thrust fault, Seismology and Chronology.
He has included themes like Glacial period, Aggradation and Sedimentary rock, Structural basin, Clastic rock in his Pleistocene study. His research in Sediment intersects with topics in Syntaxis, Floodplain, Plateau and Massif. His studies deal with areas such as Fault scarp, Erosion and Mountain formation as well as Denudation.
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Active folding of fluvial terraces across the Siwaliks Hills, Himalayas of central Nepal
J. Lavé;J. P. Avouac.
Journal of Geophysical Research (2000)
Fluvial incision and tectonic uplift across the Himalayas of central Nepal
J. Lavé;J. P. Avouac.
Journal of Geophysical Research (2001)
Interseismic strain accumulation on the Himalayan crustal ramp (Nepal)
M. R. Pandey;R. P. Tandukar;J. P. Avouac;J. Lavé.
Geophysical Research Letters (1995)
Evidence for a great medieval earthquake (~1100 A.D.) in the central Himalayas, Nepal.
J. Lavé;D. Yule;S. Sapkota;K. Basant.
Science (2005)
Late Cenozoic evolution of the central Longmen Shan, eastern Tibet: Insight from (U-Th)/He thermochronometry
Vincent Godard;Vincent Godard;R Pik;J Lavé;J Lavé;R Cattin;R Cattin.
Tectonics (2009)
Changes of bedload characteristics along the Marsyandi River (central Nepal): Implications for understanding hillslope sediment supply, sediment load evolution along fluvial networks, and denudation in active orogenic belts
Mikaël Attal;Jérôme Lavé.
Geological Society of America Special Papers (2006)
Predominant floodplain over mountain weathering of Himalayan sediments (Ganga basin)
Maarten Lupker;Christian France-Lanord;Valier Galy;Jérôme Lavé.
Geochimica et Cosmochimica Acta (2012)
Stability of the Upper Nile drainage network (Ethiopia) deduced from (U–Th)/He thermochronometry: implications for uplift and erosion of the Afar plume dome
Raphaël Pik;Bernard Marty;Bernard Marty;Jean Carignan;Jérôme Lavé.
Earth and Planetary Science Letters (2003)
Increasing chemical weathering in the Himalayan system since the Last Glacial Maximum
Maarten Lupker;Christian France-Lanord;Valier Galy;Jérôme Lavé.
Earth and Planetary Science Letters (2013)
Investigation of the relationships between basin morphology, tectonic uplift, and denudation from the study of an active fold belt in the Siwalik Hills, central Nepal
J.-E. Hurtrez;J.-E. Hurtrez;F. Lucazeau;F. Lucazeau;J. Lavé;J.-P. Avouac.
Journal of Geophysical Research (1999)
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