Mountain building processes at the orogenic front: A study of the unroofing in Neogene foreland sequence (37°S) Procesos orogénicos en el frente Andino: Estudio de una secuencia de destechado correspondiente a la cuenca de antepaís neógena

Autor: Lucía Sagripanti, Germán Bottesi, Diego Kietzmann, Andrés Folguera, Víctor A Ramos

Publikováno v: Andean Geology, Vol 39, Iss 2, Pp 201-219 (2012)

The orogenic front at 37°S has been mainly formed through at least two contraccional stages, as inferred from the exhumed major angular unconformities at the Late Eocene and the Late Miocene times respectively. A Late Cretaceous event is restricted

Externí odkaz: https://doaj.org/article/0045683536994ad4be069388171e6e7f

Tectonosedimentary evolution of the Coastal Cordillera and Central Depression of south-Central Chile (36°30′-42°S)

Autor: J. Otero, A. Anavalón, Lucía Sagripanti, Victor A. Valencia, M.P. Rodríguez, P. Giroux, D. Orts, Andrés Echaurren, Patricio Zambrano, Alfonso Encinas

Publikováno v: CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
RID-UNRN (UNRN)
Universidad Nacional de Río Negro
instacron:UNRN

Fil: Encinas, Alfonso. Universidad de Concepción, Facultad de Ciencias Químicas, Departamento de Ciencias de la Tierra, Concepción, Chile Fil: Sagripanti, Lucía. Universidad de Buenos Aires, CONICET, Instituto de Estudios Andinos "Don Pablo Groeb

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::336c3ccf4f15603ec73c6e987787c753
https://www.sciencedirect.com/science/article/abs/pii/S0012825220305110?via=ihub

Quaternary tectonics in the southern Central Andes (37°-38° S): Retroarc compression inferred from morphotectonics and numerical models

Autor: Carlos H. Costa, Andrés Folguera, Bruno Colavitto, Lucía Jagoe, Lucía Sagripanti

A neotectonic study at the transitional segment between the Central and North Patagonian Andes, in the northern part of the Neuquén province in Argentina (37°-38°S) was carried out revisiting sites previously surveyed and addressing new field evid

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d982837b451b9849bbff7d4e549a1282
https://linkinghub.elsevier.com/retrieve/pii/S0895981120302406

A review about the quaternary upper-plate deformation in the Southern Central Andes (36–38°S): A plausible interaction between mantle dynamics and tectonics

Autor: Carlos H. Costa, Lucía Jagoe, Lucía Sagripanti, Folguera Andres, Bruno Colavitto

Publikováno v: Journal of South American Earth Sciences. 87:221-231

Quaternary deformation in the Southern Central Andes between 36° and 38°S is disconnected, noncontinuous and not particularly tracing the main mountain topographic fronts. This pattern contrasts to the one to the north through the Chilean-Pampean f

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0082ac22a7d5d8e3ec21e4402928a1fb
https://doi.org/10.1016/j.jsames.2017.11.008

Tectonics Associated with the Late Oligocene to Early Miocene Units of the High Andes (Cura-Mallín Formation). A Review of the Geochronological, Thermochronological, and Geochemical Data

Autor: Vanesa D. Litvak, Darío Orts, Sofía B. Iannelli, Andrés Folguera, Eduardo Agustín Rosselot, Lucía Sagripanti, Alfonso Encinas, María Hurley, Lucas Fennell

Publikováno v: Opening and Closure of the Neuquén Basin in the Southern Andes ISBN: 9783030296797
Opening and Closure of the Neuquén Basin in the Southern Andes

The tectonic regime associated with the Oligo-Miocene Cura-Mallín Formationand equivalents in the Main Andean Cordillera between 35° and 40° S, theVentana and Abanico formations to the south and north, respectively, is still matter of debate. Whil

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b7da9ff9c63f064e5dd30e227c471814
https://doi.org/10.1007/978-3-030-29680-3_18