Structure and Cenozoic evolution of Western Cuba fold and thrust belt
Núm. 30, International Meeting of Young Researchers in Structural Geology and Tectonics (Part 2)
Núm. 30

Structure and Cenozoic evolution of Western Cuba fold and thrust belt

International Meeting of Young Researchers in Structural Geology and Tectonics (Part 2)
  • E. Saura
  • J. Vergés
  • D. Brown
  • P. Lukito
  • S. Soriano
  • S. Torrescusa
  • R. García
  • J. R. Sánchez
  • C. Sosa
  • R. Tenreyro
E. Saura
J. Vergés
D. Brown
P. Lukito
S. Soriano
S. Torrescusa
R. García
J. R. Sánchez
C. Sosa
R. Tenreyro
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Saura, E., Vergés, J., Brown, D., Lukito, P., Soriano, S., Torrescusa, S., García, R., Sánchez, J. R., Sosa, C., & Tenreyro, R. (2011). Structure and Cenozoic evolution of Western Cuba fold and thrust belt. Trabajos De Geología, 30(30). Recuperado a partir de https://reunido.uniovi.es/index.php/TDG/article/view/184
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Resumen

We present balanced and restored cross-sections across the Western Cuba fold and thrust belt,based on MCS profiles, field data and balancing techniques. The cross-section intersects the Los PalaciosBasin, the Sierra del Rosario antiformal stack, the Bahía Honda unit, the frontal imbricated thrustsheets, the foredeep basin and a buried, geometrically inferred duplex. The minimum calculated shorteningis 130 km. Syntectonic deposits and a forward kinematic model provide a good constraint for theCenozoic tectonic evolution of the orogen, from the emplacement of the Bahía Honda unit to the finalinfill of the foredeep.
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