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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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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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Darin A. Croft,Juan P. Radic,Enrique Zurita,Reynaldo Charrier,John J. Flynn,Andre R. Wyss
Pág. 285 - 298
Middle Miocene fluvo-lacustrine strata of the Río Pedregoso Member of the Cura-Mallín Formation are broadly exposed to the east and south of the town of Lonquimay, Chile. These strata accumulated in the extensional Cura-Mallín Basin, a basin which was su...
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Nelson Munoz,Reynaldo Charrier,Teresa Jordan
Pág. 55 - 80
A reinterpretation of the structural style on the eastern Cordillera Domeyko and the adjacent Salar de Atacama Basin reveals the existence of west-dipping, high-angle, thrust-faults extending below the Cordillera Domeyko and Cordón de Lila, resulting fro...
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Andrew C. Kurtz,Suzanne M. Kay,Reynaldo Charrier,Edward Farrar
Pág. 75 - 90
ABSTRACT. 40Ar/39Ar mineral dating and whole rock chemical analyses of Miocene to Pliocene Andean granitoids near the El Teniente copper deposit (34°S) provide new evidence for rapid Neogene exhumation. This exhumation is attributed to crustal thickening...
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Andrew C. Kurtz,Suzanne M. Kay,Reynaldo Charrier,Edward Farrar
Pág. 75 - 90
ABSTRACT. 40Ar/39Ar mineral dating and whole rock chemical analyses of Miocene to Pliocene Andean granitoids near the El Teniente copper deposit (34°S) provide new evidence for rapid Neogene exhumation. This exhumation is attributed to crustal thickening...
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Sofia Rebolledo,Reynaldo Charrier
Pág. 55 - 69
RESUMEN. Las unidades paleozoicas que afloran en la costa de Chile central son: el Complejo Metamorfico del Choapa (CMC) y las formaciores Puerto Manso y Huentelauquen. El CMC, cuyo protolito consistio en grauwacas, arcosas y basaltos oceanicos, esta con...
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Sofia Rebolledo,Reynaldo Charrier
Pág. 55 - 69
RESUMEN. Las unidades paleozoicas que afloran en la costa de Chile central son: el Complejo Metamorfico del Choapa (CMC) y las formaciores Puerto Manso y Huentelauquen. El CMC, cuyo protolito consistio en grauwacas, arcosas y basaltos oceanicos, esta con...
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Charles R. Stern,Hassan Amini,Reynaldo Charrier,Estanislao Godoy,Francisco Herve,Juan Varela
RESUMEN:Se estudiaron cuarenta y cinco muestras de pomez recogidas en distintos afloramientos de flujos piroclasticos, en la Depresion Longitudinal, en la Cordillera de la Costa y la vertiente occidental de la Cordillera Principal a lo largo de los valle...
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Reynaldo Charrier
RESUMEN:Los antecedentes cronologicos y los caracteres litologicos y de facies de la parte superior, calcarea y marina, de la secuencia definida por Klohn (1960) como Formacion Lenas-Espinoza, permiten asignarla a la Formacion Banos del Flaco. Se restrin...
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Reynaldo Charrier
RESUMEN:Se da a conocer el descubrimiento de dos centros volcanicos en la Cordillera de los Andes, entre 34°y 34°45' de latitud sur, los volcanes Andres, ubicado a 4,5 km al NE del volcan Palomo, y Don Casimiro, ubicado a unos 5 km al SW del volcan Maipo...
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Reynaldo Charrier,Francisco Munizaga
RESUMEN:Se presentan los resultados de 9 analisis radiometricos K-Ar practicados en rocas volcanicas, principalmente andesiticas, pertenecientes a las Formaciones Coya-Machali y Farellones y a coladas de valle, que afloran en el borde occidental de la Co...
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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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