The evolution of the Cenozoic deformation of the Cordillera Oriental and of the contact zone with the Altiplano in southern Bolivia is well documented in the Tupiza, Nazareno and Estarca basins. The tectonic evolution started at about 29 Ma. The period between 29 and about 22-21 Ma is marked by developement of a pull-apart basin related to N-S trending left-lateral strike-slip faulting. During this period, initial deposition consisted of andesitic lavas and detrital sediments (breccias ; matrix-supported red conglomerats ; sands and silts...) of the Catati and Tupiza Formation, deposited in alluvial fan and flood plain environments. From 21 to 20 Ma, the tectonic setting evolved to N-S oriented thrusts, which had a dextral component. This e...
The central Andean retroarc thrust belt is characterized by a southward transition at ∼22°S in struc...
Late Cenozoic Andean deformation in the Pampean segment of Argentina and Chile (27°00′-33°30′S) prov...
Formation of the Bolivian eastern cordillera started at the end of the Oligocene and continues to th...
Recent advances in biochrology, geochrology, magnetostratigraphy, structural geology, and basin anal...
Temporal-spatial evolution of the Central Andean foreland basin system relates directly to growth of...
Integrated studies of stratigraphy, sedimentology, paleogeography and tectonic controls on Cenozoic ...
Summarization: The Eastern Cordillera of southern Bolivia is situated between the Altiplano high pla...
Evolution of the Subandean fold-thrust belt and adjacent Chaco foreland basin since their inception ...
Fault systems observed in the southernmost Peruvian forearc (Tacna area) provide information on the ...
The Central Andes are the product of contractional deformation related to subduction of the Nazca pl...
The Andean internal zone records deformation, uplift and erosion that serve as proxies of variations...
The Andes are an ideal setting to explore orogenic wedge evolution and the cyclical tectonic process...
Artículo de publicación ISIA review of available stratigraphic, structural, and magmatic evolution ...
The evolution of Neogene Central Andes is characterized by the eastward propagation of deformation f...
Cenozoic shortening in the central Andes of southern Peru was accommodated by thin- and thick-skinne...
The central Andean retroarc thrust belt is characterized by a southward transition at ∼22°S in struc...
Late Cenozoic Andean deformation in the Pampean segment of Argentina and Chile (27°00′-33°30′S) prov...
Formation of the Bolivian eastern cordillera started at the end of the Oligocene and continues to th...
Recent advances in biochrology, geochrology, magnetostratigraphy, structural geology, and basin anal...
Temporal-spatial evolution of the Central Andean foreland basin system relates directly to growth of...
Integrated studies of stratigraphy, sedimentology, paleogeography and tectonic controls on Cenozoic ...
Summarization: The Eastern Cordillera of southern Bolivia is situated between the Altiplano high pla...
Evolution of the Subandean fold-thrust belt and adjacent Chaco foreland basin since their inception ...
Fault systems observed in the southernmost Peruvian forearc (Tacna area) provide information on the ...
The Central Andes are the product of contractional deformation related to subduction of the Nazca pl...
The Andean internal zone records deformation, uplift and erosion that serve as proxies of variations...
The Andes are an ideal setting to explore orogenic wedge evolution and the cyclical tectonic process...
Artículo de publicación ISIA review of available stratigraphic, structural, and magmatic evolution ...
The evolution of Neogene Central Andes is characterized by the eastward propagation of deformation f...
Cenozoic shortening in the central Andes of southern Peru was accommodated by thin- and thick-skinne...
The central Andean retroarc thrust belt is characterized by a southward transition at ∼22°S in struc...
Late Cenozoic Andean deformation in the Pampean segment of Argentina and Chile (27°00′-33°30′S) prov...
Formation of the Bolivian eastern cordillera started at the end of the Oligocene and continues to th...