Summary
High-standing orogenic plateaus are key features of most mountainous regions, and typically have profound regional, and in many cases global, impacts on atmospheric circulation and precipitation patterns. The Colorado Plateau is characterized by a low-relief surface at high elevation and deep canyon incision at the plateau margins. Although these canyons are key features of ecosystems and water resources, the chronology of the uplift and subsequent canyon incision remains debated. In addition, the relative importance of deep-seated processes, changes in paleogeography and climate, on the late geomorphologic evolution of the plateau remains controversial. Two endmember models of Grand Canyon incision have been proposed: a 80-60 Ma incision or a 6-5 Ma incision, the discrepancy between these models is partly related to limitations in conventional thermochronology techniques. This project will provide new constraints on the incision history of the canyons carved across the Colorado Plateau using an innovative set of thermochronometers. I will combine apatite (U-Th-Sm)/He and fission-track data to document the thermal history of rocks in Zion Canyon which has never been explored and infer the respective effects of erosion and regional magmatism on the thermal evolution of the lithosphere. Electron spin resonance (ESR) thermochronometry, a new thermochronometer sensitive to temperature ranging from 50 to 20˚C will be performed on the same samples and combined with thermo-kinematic modelling to decipher the timing and rate of canyon incision in Zion. Finally, I will apply ESR thermochronometry in selected canyons to decipher the timing of incision across the Colorado Plateau. Low-temperature thermochronology data, including ESR, will be integrated in a numerical model of the landscape evolution to test different processes (change in base level versus mantellic process) and associated scenarios for the Colorado Plateau uplift and incision.
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| Web resources: | https://cordis.europa.eu/project/id/101066908 |
| Start date: | 01-07-2023 |
| End date: | 30-06-2026 |
| Total budget - Public funding: | - 308 746,00 Euro |
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Original description
High-standing orogenic plateaus are key features of most mountainous regions, and typically have profound regional, and in many cases global, impacts on atmospheric circulation and precipitation patterns. The Colorado Plateau is characterized by a low-relief surface at high elevation and deep canyon incision at the plateau margins. Although these canyons are key features of ecosystems and water resources, the chronology of the uplift and subsequent canyon incision remains debated. In addition, the relative importance of deep-seated processes, changes in paleogeography and climate, on the late geomorphologic evolution of the plateau remains controversial. Two endmember models of Grand Canyon incision have been proposed: a 80-60 Ma incision or a 6-5 Ma incision, the discrepancy between these models is partly related to limitations in conventional thermochronology techniques. This project will provide new constraints on the incision history of the canyons carved across the Colorado Plateau using an innovative set of thermochronometers. I will combine apatite (U-Th-Sm)/He and fission-track data to document the thermal history of rocks in Zion Canyon which has never been explored and infer the respective effects of erosion and regional magmatism on the thermal evolution of the lithosphere. Electron spin resonance (ESR) thermochronometry, a new thermochronometer sensitive to temperature ranging from 50 to 20˚C will be performed on the same samples and combined with thermo-kinematic modelling to decipher the timing and rate of canyon incision in Zion. Finally, I will apply ESR thermochronometry in selected canyons to decipher the timing of incision across the Colorado Plateau. Low-temperature thermochronology data, including ESR, will be integrated in a numerical model of the landscape evolution to test different processes (change in base level versus mantellic process) and associated scenarios for the Colorado Plateau uplift and incision.Status
SIGNEDCall topic
HORIZON-MSCA-2021-PF-01-01Update Date
09-02-2023
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