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Projekt Druckansicht

Einfluss von Tektonik, Klima und Erosion auf das Einschneiden und die Breite des Andenplateaus, Südperu

Antragstellerin Dr. Sarah Falkowski
Fachliche Zuordnung Paläontologie
Förderung Förderung von 2017 bis 2021
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 363550969
 
Erstellungsjahr 2023

Zusammenfassung der Projektergebnisse

In this collaborative project, we contributed across-strike data on (i) timing and magnitude of exhumation, (ii) structural geometries, and (iii) thermokinematic histories to evaluate drivers of eastern Andean Plateau exhumation and incision. Results show that the first-order thermochronometric age pattern is a function of rocks' vertical and lateral movement over basement ramps and resulting exhumational erosion. This pattern is superimposed with a regional and synchronous incision-related exhumation signal since the Pliocene. While this incision occurred independent of structural deformation, the exhumation magnitude and difference in interfluve and canyon thermochronometric ages require the presence of a tectonic contribution to exhumation. We conclude that uplift over a basement ramp in the Eastern Cordillera and a decrease in shortening rates since ~10 Ma set the stage for climate-enhanced incision to occur in southern Peru. Overall, I deem the project a success. The strength of this project was the combined expertise from different disciplines, broad sampling approach, and integration of various datasets. Our findings will guide future research in the eastern Central Andes and impact similar studies elsewhere. In most parts, the project developed according to plan. In parts, progress was slowed down by the corona pandemic, which particularly affected the analytical portion of the US collaborators' project. However, independent of that slowdown, the timely completion of all the project goals would have been more achievable with one less transect.

Projektbezogene Publikationen (Auswahl)

 
 

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