Paleozoic to present-day kinematic evolution of the frontal part of the Andes between parallels 23º and 24º S (Jujuy province, Argentina)
Núm. 30, International Meeting of Young Researchers in Structural Geology and Tectonics (Part 2)
Núm. 30

Paleozoic to present-day kinematic evolution of the frontal part of the Andes between parallels 23º and 24º S (Jujuy province, Argentina)

International Meeting of Young Researchers in Structural Geology and Tectonics (Part 2)
  • R. E. Seggiaro
  • M. Bulnes
  • J. Poblet
  • N. G. Aguilera
  • L. R. Rodríguez-Fernández
  • N. Heredia
  • J. L. Alonso
R. E. Seggiaro
M. Bulnes
J. Poblet
N. G. Aguilera
L. R. Rodríguez-Fernández
N. Heredia
J. L. Alonso
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Cómo citar

Seggiaro, R. E., Bulnes, M., Poblet, J., Aguilera, N. G., Rodríguez-Fernández, L. R., Heredia, N., & Alonso, J. L. (2011). Paleozoic to present-day kinematic evolution of the frontal part of the Andes between parallels 23º and 24º S (Jujuy province, Argentina). Trabajos De Geología, 30(30). Recuperado a partir de https://reunido.uniovi.es/index.php/TDG/article/view/186
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Resumen

A geological map and a transect across the thick-skinned Eastern Cordillera and the transitionbetween the thin-skinned Subandean Ranges and the thick-skinned Santa Barbara System (all ofthem NNE-SSW striking) interfered by the NE-SW trending rift called Lomas the Olmedo Trough,at a latitude comprised between 23º S and 24° S, were constructed. The available data allowed us toillustrate the geometry and the kinematic evolution of the structures formed during three main tectonicevents recorded in this region: a Cenozoic contractional event (Andean orogeny), an extensionalCretaceous event and a Paleozoic event (?).
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