Page 1. 6th International Symposium on Andean Geodynamics (ISAG 2005, Barcelona), Extended Abstra... more Page 1. 6th International Symposium on Andean Geodynamics (ISAG 2005, Barcelona), Extended Abstracts: 273-276 273 Exhumation and uplift of the western Main Cordillera between 33º and 34ºS Andrés Fock 1, Reynaldo ...
Extensional basin development (Middle?-Late Eocene to Early Miocene), basin inversion and deforma... more Extensional basin development (Middle?-Late Eocene to Early Miocene), basin inversion and deformation of the basin fill (Early to Late Miocene) and rapid, high magnitude surface uplift (Late Miocene to Recent) characterize the Cenozoic tectonic evolution of the central Chilean Principal Cordillera, between 33° and 36°S. Extension (Abanico Basin) was associated with crustal thinning and toleiitic magmatism, while basin inversion was
Page 1. 6th International Symposium on Andean Geodynamics (ISAG 2005, Barcelona), Extended Abstra... more Page 1. 6th International Symposium on Andean Geodynamics (ISAG 2005, Barcelona), Extended Abstracts: 273-276 273 Exhumation and uplift of the western Main Cordillera between 33º and 34ºS Andrés Fock 1, Reynaldo ...
Extensional basin development (Middle?-Late Eocene to Early Miocene), basin inversion and deforma... more Extensional basin development (Middle?-Late Eocene to Early Miocene), basin inversion and deformation of the basin fill (Early to Late Miocene) and rapid, high magnitude surface uplift (Late Miocene to Recent) characterize the Cenozoic tectonic evolution of the central Chilean Principal Cordillera, between 33° and 36°S. Extension (Abanico Basin) was associated with crustal thinning and toleiitic magmatism, while basin inversion was
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