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Reynaldo Charrier
Pág. 463 - 465
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Matías Villarroel,Pamela Jara,Reynaldo Charrier
Pág. 153 - 174
Lithological heterogeneities in a rock series deformed by the development of a fold-and-thrust belt (FTB) affects the pattern of the resulting structures. We present a series of analogue experiments to determine the effect caused on the deformation patte...
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Reynaldo Charrier,Estanislao Godoy,Francisco Hervé,Claudio Parica
Pág. 466 - 467
Prof. Hubert Miller passed away February 26, 2020, near his hometown München in Bavaria.
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Reynaldo Charrier,Lasafam Iturrizaga,Sébastien Carretier,Vincent Regard
Pág. 240 - 278
We present here a reconstruction of the post late Miocene landscape evolution of the western slope of the Andean Cordillera Principal near 34°20? S. We base our analysis on the available geological information, a morphological characterization of the lan...
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Carolina Muñoz-Sáez,Luisa del Carmen Pinto,Reynaldo Charrier,Thierry Nalpas
Pág. 1 - 28
The current paper analyzes the evolution of the Abanico Basin, exposed in the Chilean Principal Cordillera in central Chile (33º-35ºS). According to previous studies, the basin has been affected by two main deformational episodes; the first, related to e...
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Pamela Jara,Reynaldo Charrier
Pág. 174 - 209
New stratigraphical and geochronological constraints for the Mezo-Cenozoic deposits in the High Andes of central Chile between 32° and 32°30?S: Structural and palaeogeographic implications. Attempts to differentiate geological units of the Andean Princip...
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Pablo Rossel,Veronica Oliveros,José Mescua,Felipe Tapia,Mihai Nicolae Ducea,Sergio Calderón,Reynaldo Charrier,Derek Hoffman
Pág. 529 - 557
The uppermost Jurassic continental and volcanic deposits of the Río Damas-Tordillo Formation represent an interval of intense continental deposition within the Jurassic to Early Cretaceous dominantly marine environment of the Mendoza-Neuquén back-arc bas...
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Jose Piquer,Juan Carlos Castelli,Reynaldo Charrier,Gonzalo Yanez
Pág. 32 - 53
The Cenozoic geologic evolution of the central part of the Cordillera Principal at ~35°S, is intimately related to the geodynamic evolution of deep crustal structures, which during different stages controlled the deposition of volcanosedimentary sequence...
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Victor Maksaev,Francisco Munizaga,Marcos Zentilli,Reynaldo Charrier
Pág. 153 - 171
Apatite fission track data for Miocene plutons of the western slope of the Principal Andean Cordillera in central Chile (33-35°S) define a distinct episode of enhanced crustal cooling through the temperature range of the apatite partial annealing zone (~...
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Luisa Pinto,Gerard Herail,Reynaldo Charrier
Pág. 19 - 44
In northern Chile (18-20°S), the western border of the high Andean Plateau (Altiplano) was uplifted by high-angle thrust faults and associated folds. These developed along the Precordillera, which is the morphostructural unit that connects the Andean Pla...
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