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Kinematic variations across Eastern Cordillera at 24°S (Central Andes): tectonic and magmatic implications
(Elsevier Science, 2007-04)
The Eastern Cordillera (Central Andes, ∼ 24°S) consists of a basement-involved thrust system, resulting from Miocene-Quaternary eastward migrating compression, separating the Puna plateau from the Santa Barbara System ...
The Cononodont Trapezognathus Diprion (Lindström) in the Acoite Formation, Eastern Cordillera, Northwestern Argentina
(Asociación Paleontológica Argentina, 2013-07)
This work is developed in NW Argentina framed in the geological province of the Eastern Cordillera, characterized by a set of siliciclastic outcrops mainly related to the Cambrian and Ordovician periods. The main purpose ...
The Quebrada de Humahuaca area and the Eastern Border of the Eastern Cordillera, Jujuy province
(Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Instituto Superior de Correlación Geológica, 2003)
The southern half of the Eastern Cordillera is divided into three areas, limited by important tectonic fronts: the Eastern Zone, the Maximum Imbrication Zone and the Western Zone (Figure 6). In all of them there appear ...
The Mojotoro Range, eastern cordillera, Salta province
(Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Instituto Superior de Correlación Geológica, 2003)
The Mojotoro Range (MR) is located at the SE end of the Argentine Eastern Cordillera, to the east of Salta City (Figure 7a,b). From a structural point of view, the MR is a complex anticlinorioum of N–S strike that closes ...
A new species of cyrtochilum (orchidaceae: oncidiinae) from the eastern cordillera of Colombia
(Lankester Botanical Garden, University of Costa Rica, 2018)
Late Cambrian – Tremadocian faunas and events from Angosto del Moreno Section, Eastern Cordillera, Argentina
(Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Instituto Superior de Correlación Geológica, 2003)
The Santa Victoria Group (SVG, late Upper Cambrian – Caradocian) comprises pre–Ashgillian Ordovician deposits of the Argentinean Eastern Cordillera. The most significant section of the SVG in the western flank of the Eastern ...
Comments on "Kinematic variations across Eastern Cordillera at 24°S (Central Andes): Tectonic and magmatic implications" by Acocella, et al. [Tectonophysics 434 (2007) 81-92]
(Elsevier Science, 2009-04)
The interpretation of Acocella et al. about (i) westward increase of strike-slip motion, (ii) strain partitioning, (iii) symmetry of the Central Andes, as well as (iv) the interpreted cause for the occurrence of magmatic ...
Reply to comment on "Kinematic variations across Eastern Cordillera at 24°S (Central Andes): Tectonic and magmatic implications"
(Elsevier Science, 2009-04)
We discuss in detail all the comments made by Petrinovic et al., showing that these are not pertinent to the aim of our study, or based on incomplete information of fault kinematics, or unsupported. Despite our limited ...