Detailseite
Projekt Druckansicht

Vulkanotektonik in transpressiven magmatischen Bögen

Fachliche Zuordnung Paläontologie
Förderung Förderung von 2018 bis 2022
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 355640964
 
Erstellungsjahr 2022

Zusammenfassung der Projektergebnisse

Field-based, remote sensing and experimental work complemented by a reassessment of published thermochronological and GPS data highlight the success of the bilateral DFG-MINCYT/CONICET project. Notably, transpression affected the entire width of the Southern Andes and was accomplished by distributed deformation. The location of Copahue volcanoe appears to be genetically unrelated to crustal faults but may have formed as a consequence of local dilation due to perturbation of principal stresses. Contrary to previous studies, Caviahue caldera unlikely originated as a tectonic pull-apart basin, and NW-striking faults may well have formed early in Andean orogenesis. The project sets the stage for a larger collaborative research effort geared towards understanding the role of crustal flow perturbations in volcano-tectonically active areas.

Projektbezogene Publikationen (Auswahl)

  • 2021. Editorial - From Proterozoic tectonics to Quaternary climate variability: Earth system science studies in Latin America. International Journal of Earth Sciences 110, 2269–2271
    Riller, U., Giambiagi, L., Strecker, M.R.
    (Siehe online unter https://doi.org/10.1007/s00531-021-02095-9)
  • 2021. Kinematic partitioning in the Southern Andes (39° S–46° S) inferred from lineament analysis and reassessment of exhumation rates. International Journal of Earth Science 110, 2385–2398
    Göllner, P.L., Eisermann, J.O., Balbis, C., Petrinovic, I.A., Riller, U.
    (Siehe online unter https://doi.org/10.1007/s00531-021-02068-y)
  • 2021. Orogen-scale transpression accounts for GPS velocities and kinematic partitioning in the Southern Andes. Communications Earth & Environment 2, 167
    Eisermann, J.O., Göllner, P.L., Riller, U.
    (Siehe online unter https://doi.org/10.1038/s43247-021-00241-4)
  • 2021. Unraveling the timing of the Caviahue depression, Andean Southern Volcanic Zone: insights from the sedimentary infill. International Journal of Earth Sciences 110, 2541–2558
    Hernando, I.R., Bucher, J., del Papa, C.E., Eisermann, J.O., Göllner, P.L., Guzmán, S.R., Balbis, C., Petrinovic, I.A.
    (Siehe online unter https://doi.org/10.1007/s00531-020-01936-3)
 
 

Zusatzinformationen

Textvergrößerung und Kontrastanpassung