Since the early 90's, the coupling and interaction between tectonics, climate and surface processes have been a key question in the Geosciences community. Here, the recent relief evolution of the Ecrins-Pelvoux massif (French Western Alps) induced by Pleistocene / Holocene climate change is studied using in-situ produced Terrestrial Cosmogenic Nuclide (TCN) measurements that have been performed on more than 60 samples consisting of both bedrock and detrital material. 10Be and 26Al measurements performed on samples collected from glacial features (glacially polished bedrock, roches moutonnées, nunataks) allow constraining both the chronology and pattern of ice retreat within the massif. Cosmic-ray exposure dating shows a contrasting response...
The topographic evolution of mountain belts results from complex couplings between tectonics, climat...
The interaction between the intermediate water masses and rapid climate changes is becoming a hottop...
The topographic evolution of mountain belts results from complex couplings between tectonics, climat...
Since the early 90's, the coupling and interaction between tectonics, climate and surface processes ...
Since the early 90's, the coupling and interaction between tectonics, climate and surface processes ...
The global warming observed since the beginning of the last century, and mostly attributed to the si...
The topographic evolution of mountain belts results from complex couplings between tectonics, climat...
Building materials of historical monuments, such as natural stone, are subject to aggressive environ...
The study presented in this PhD memory aim at better define and quantify the present timeerosion pro...
Thèse soutenue devant le jury composé de : Philippe DAVY Président Philippe BELLEUDY Rapporteur Niel...
Thèse soutenue devant le jury composé de : Philippe DAVY Président Philippe BELLEUDY Rapporteur Niel...
The study presented in this PhD memory aim at better define and quantify the present timeerosion pro...
The study presented in this PhD memory aim at better define and quantify the present timeerosion pro...
The study presented in this PhD memory aim at better define and quantify the present timeerosion pro...
The topographic evolution of mountain belts results from complex couplings between tectonics, climat...
The topographic evolution of mountain belts results from complex couplings between tectonics, climat...
The interaction between the intermediate water masses and rapid climate changes is becoming a hottop...
The topographic evolution of mountain belts results from complex couplings between tectonics, climat...
Since the early 90's, the coupling and interaction between tectonics, climate and surface processes ...
Since the early 90's, the coupling and interaction between tectonics, climate and surface processes ...
The global warming observed since the beginning of the last century, and mostly attributed to the si...
The topographic evolution of mountain belts results from complex couplings between tectonics, climat...
Building materials of historical monuments, such as natural stone, are subject to aggressive environ...
The study presented in this PhD memory aim at better define and quantify the present timeerosion pro...
Thèse soutenue devant le jury composé de : Philippe DAVY Président Philippe BELLEUDY Rapporteur Niel...
Thèse soutenue devant le jury composé de : Philippe DAVY Président Philippe BELLEUDY Rapporteur Niel...
The study presented in this PhD memory aim at better define and quantify the present timeerosion pro...
The study presented in this PhD memory aim at better define and quantify the present timeerosion pro...
The study presented in this PhD memory aim at better define and quantify the present timeerosion pro...
The topographic evolution of mountain belts results from complex couplings between tectonics, climat...
The topographic evolution of mountain belts results from complex couplings between tectonics, climat...
The interaction between the intermediate water masses and rapid climate changes is becoming a hottop...
The topographic evolution of mountain belts results from complex couplings between tectonics, climat...