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dc.contributor.author
Gianni, Guido Martin  
dc.contributor.author
Folguera Telichevsky, Andres  
dc.contributor.author
Navarrete, César  
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Encinas, Alfonso  
dc.contributor.author
Echaurren Gonzalez, Andres  
dc.contributor.other
Folguera Telichevsky, Andres  
dc.contributor.other
Naipauer, Maximiliano  
dc.contributor.other
Sagripanti, Lucía  
dc.contributor.other
Ghiglione, Matias  
dc.contributor.other
Orts, Darío Leandro  
dc.contributor.other
Giambiagi, Laura Beatriz  
dc.date.available
2022-04-12T17:23:38Z  
dc.date.issued
2015  
dc.identifier.citation
Gianni, Guido Martin; Folguera Telichevsky, Andres; Navarrete, César; Encinas, Alfonso; Echaurren Gonzalez, Andres; The North Patagonian Orogen: Meso-Cenozoic Evolution from the Andes to the Foreland Area; Springer; 2015; 300-350  
dc.identifier.isbn
978-3-319-23059-7  
dc.identifier.uri
http://hdl.handle.net/11336/155062  
dc.description.abstract
In the last decades an important amount of studies have dealt with the Patagonian orogen. However, an holistic approach on the evolution of this sector has not been addressed yet. A review of recent advances in different geological aspects of the Patagonian orogen and its related broken foreland system, reveals a clear correlation between the geological evolution of both sectors. This enabled us to integrate them in an evolutionary model connecting tectonic events from the North Patagonian Andes to the broken foreland area throughout the Mesozoic to Cenozoic era. During the break-up of Western Gondwana, beginning in Jurassic times, several extensional basins developed in the Patagonian region. In late Early Cretaceous to Paleocene, a switch in the tectonic regime caused the uplift of the North Patagonian Andes and the initial fragmentation of the foreland area. Synchronously an eastward magmatic arc migration is documented at the retroarc area. At this moment, a series of mid-ocean ridges collided one after another against the patagonian margin. A causative relation among young lithosphere subduction, slab shallowing, orogenesis and eruption of anomalous orogenesis at the arc and retroarc region has been proposed. In concert to regional compression, synorogenic foreland rifting occurred transversaly to the main andean trend in the San Jorge Gulf Basin, describing an exeptional setting for this type of rifting mechanism. From Eocene to early Miocene westward definition of the magmatic arc, possibly related to roll-back, opened the highly attenuated Traiguen Basin, splitted the arc and forearc area. To the east, extensive intraplate magmatism began in the patagonian foreland collapsing the broken foreland orogen. During the Neogene, an acceleration of the convergence rate caused the renewal of Patogonian Andes orogenesis and reactivation the broken foreland system. Orogenesis along with Late Cenozoic global cooling triggered aridization in the foreland zone which had dramatic consequences for the patagonian fauna and flora.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Springer  
dc.rights
info:eu-repo/semantics/restrictedAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
North Patagonian Andes  
dc.subject
broken foreland  
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San jorge Gulf Basin  
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mid-ocean ridge  
dc.subject.classification
Geología  
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Ciencias de la Tierra y relacionadas con el Medio Ambiente  
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CIENCIAS NATURALES Y EXACTAS  
dc.title
The North Patagonian Orogen: Meso-Cenozoic Evolution from the Andes to the Foreland Area  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.type
info:eu-repo/semantics/bookPart  
dc.type
info:ar-repo/semantics/parte de libro  
dc.date.updated
2022-03-31T18:44:04Z  
dc.journal.pagination
300-350  
dc.journal.pais
Reino Unido  
dc.journal.ciudad
Londres  
dc.description.fil
Fil: Gianni, Guido Martin. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina  
dc.description.fil
Fil: Folguera Telichevsky, Andres. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina  
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Fil: Navarrete, César. Universidad Nacional de la Patagonia "San Juan Bosco"; Argentina  
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Fil: Encinas, Alfonso. Universidad de Concepción; Chile  
dc.description.fil
Fil: Echaurren Gonzalez, Andres. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/chapter/10.1007/978-3-319-23060-3_9  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/book/10.1007/978-3-319-23060-3  
dc.conicet.paginas
474  
dc.source.titulo
Growth of the Southern Andes