Orogenias paleozoicas en los Andes de Argentina y Chile y en la península antártica
- Autores
- Heredia, Nemesio; Farias, Pedro; García-Sansegundo, Joaquín; Gallastegui, Gloria; Giacosa, Raúl; Hongn, Fernando; Tubía, José María; Alonso, Juan L.; Busquets, Pere; Charrier, Reynaldo; Clariana, María Pilar; Colombo, Ferrán; Cuesta, Andrés; Gallastegui, Jorge; Giambiagi, Laura; González Menéndez, Luis; Limarino, Carlos Oscar; Martín González, Fidel; Pedreira, David; Quintana, Luis; Rodríguez-Fernández, Luis R.; Rubio-Ordóñez, Alvaro; Seggiaro, Raúl; Serra Varela, Samanta; Spalletti, Luis Antonio; Cardó, Raúl; Ramos, Víctor A.
- Año de publicación
- 2017
- Idioma
- español castellano
- Tipo de recurso
- documento de conferencia
- Estado
- versión publicada
- Descripción
- During the late Neoproterozoic and Paleozoic, the Argentinean-Chilean Andes and, since the late Paleozoic, the Antarctic Peninsula formed part of the southwestern margin of Gondwana. During this long period of the geological time, a set of continetal fragments of variable size and allochtonie was successively accreted to that margin. This process, coupled with the development of several subductive systems, resulted in six Paleozoic orogenies, which have different temporal and spatial extensions: Pampean (Neoproterozoic-early Cambrian), Famatinian (Middle Ordovician- Silurian), Ocloyic (Middle Ordovician-Devonian), Chanic (Middle Devonian-early Carboniferous), Gondwanan (Middle Devonian-middle Permian) and Tabarin (late Permian-Triassic). All these orogenies had a collisional character, with the exception of the Tabarin and a part of the Gondwanan orogenies that are subduction-related.
Centro de Investigaciones Geológicas - Materia
-
Geología
Ocloyic orogen
Famatinian orogen
Chanic orogen
Gondwanan orogen
Tabarin orogen
Orógeno Oclóyico
Orógeno Famatiniano
Orógeno Chánico
Orógeno Gondwánico
Orógeno Tabarin - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by-nc-sa/4.0/
- Repositorio
.jpg)
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/190665
Ver los metadatos del registro completo
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Orogenias paleozoicas en los Andes de Argentina y Chile y en la península antárticaHeredia, NemesioFarias, PedroGarcía-Sansegundo, JoaquínGallastegui, GloriaGiacosa, RaúlHongn, FernandoTubía, José MaríaAlonso, Juan L.Busquets, PereCharrier, ReynaldoClariana, María PilarColombo, FerránCuesta, AndrésGallastegui, JorgeGiambiagi, LauraGonzález Menéndez, LuisLimarino, Carlos OscarMartín González, FidelPedreira, DavidQuintana, LuisRodríguez-Fernández, Luis R.Rubio-Ordóñez, AlvaroSeggiaro, RaúlSerra Varela, SamantaSpalletti, Luis AntonioCardó, RaúlRamos, Víctor A.GeologíaOcloyic orogenFamatinian orogenChanic orogenGondwanan orogenTabarin orogenOrógeno OclóyicoOrógeno FamatinianoOrógeno ChánicoOrógeno GondwánicoOrógeno TabarinDuring the late Neoproterozoic and Paleozoic, the Argentinean-Chilean Andes and, since the late Paleozoic, the Antarctic Peninsula formed part of the southwestern margin of Gondwana. During this long period of the geological time, a set of continetal fragments of variable size and allochtonie was successively accreted to that margin. This process, coupled with the development of several subductive systems, resulted in six Paleozoic orogenies, which have different temporal and spatial extensions: Pampean (Neoproterozoic-early Cambrian), Famatinian (Middle Ordovician- Silurian), Ocloyic (Middle Ordovician-Devonian), Chanic (Middle Devonian-early Carboniferous), Gondwanan (Middle Devonian-middle Permian) and Tabarin (late Permian-Triassic). All these orogenies had a collisional character, with the exception of the Tabarin and a part of the Gondwanan orogenies that are subduction-related.Centro de Investigaciones Geológicas2017-08info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionObjeto de conferenciahttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfhttp://sedici.unlp.edu.ar/handle/10915/190665spainfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2026-02-26T11:39:57Zoai:sedici.unlp.edu.ar:10915/190665Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292026-02-26 11:39:57.497SEDICI (UNLP) - Universidad Nacional de La Platafalse |
| dc.title.none.fl_str_mv |
Orogenias paleozoicas en los Andes de Argentina y Chile y en la península antártica |
| title |
Orogenias paleozoicas en los Andes de Argentina y Chile y en la península antártica |
| spellingShingle |
Orogenias paleozoicas en los Andes de Argentina y Chile y en la península antártica Heredia, Nemesio Geología Ocloyic orogen Famatinian orogen Chanic orogen Gondwanan orogen Tabarin orogen Orógeno Oclóyico Orógeno Famatiniano Orógeno Chánico Orógeno Gondwánico Orógeno Tabarin |
| title_short |
Orogenias paleozoicas en los Andes de Argentina y Chile y en la península antártica |
| title_full |
Orogenias paleozoicas en los Andes de Argentina y Chile y en la península antártica |
| title_fullStr |
Orogenias paleozoicas en los Andes de Argentina y Chile y en la península antártica |
| title_full_unstemmed |
Orogenias paleozoicas en los Andes de Argentina y Chile y en la península antártica |
| title_sort |
Orogenias paleozoicas en los Andes de Argentina y Chile y en la península antártica |
| dc.creator.none.fl_str_mv |
Heredia, Nemesio Farias, Pedro García-Sansegundo, Joaquín Gallastegui, Gloria Giacosa, Raúl Hongn, Fernando Tubía, José María Alonso, Juan L. Busquets, Pere Charrier, Reynaldo Clariana, María Pilar Colombo, Ferrán Cuesta, Andrés Gallastegui, Jorge Giambiagi, Laura González Menéndez, Luis Limarino, Carlos Oscar Martín González, Fidel Pedreira, David Quintana, Luis Rodríguez-Fernández, Luis R. Rubio-Ordóñez, Alvaro Seggiaro, Raúl Serra Varela, Samanta Spalletti, Luis Antonio Cardó, Raúl Ramos, Víctor A. |
| author |
Heredia, Nemesio |
| author_facet |
Heredia, Nemesio Farias, Pedro García-Sansegundo, Joaquín Gallastegui, Gloria Giacosa, Raúl Hongn, Fernando Tubía, José María Alonso, Juan L. Busquets, Pere Charrier, Reynaldo Clariana, María Pilar Colombo, Ferrán Cuesta, Andrés Gallastegui, Jorge Giambiagi, Laura González Menéndez, Luis Limarino, Carlos Oscar Martín González, Fidel Pedreira, David Quintana, Luis Rodríguez-Fernández, Luis R. Rubio-Ordóñez, Alvaro Seggiaro, Raúl Serra Varela, Samanta Spalletti, Luis Antonio Cardó, Raúl Ramos, Víctor A. |
| author_role |
author |
| author2 |
Farias, Pedro García-Sansegundo, Joaquín Gallastegui, Gloria Giacosa, Raúl Hongn, Fernando Tubía, José María Alonso, Juan L. Busquets, Pere Charrier, Reynaldo Clariana, María Pilar Colombo, Ferrán Cuesta, Andrés Gallastegui, Jorge Giambiagi, Laura González Menéndez, Luis Limarino, Carlos Oscar Martín González, Fidel Pedreira, David Quintana, Luis Rodríguez-Fernández, Luis R. Rubio-Ordóñez, Alvaro Seggiaro, Raúl Serra Varela, Samanta Spalletti, Luis Antonio Cardó, Raúl Ramos, Víctor A. |
| author2_role |
author author author author author author author author author author author author author author author author author author author author author author author author author author |
| dc.subject.none.fl_str_mv |
Geología Ocloyic orogen Famatinian orogen Chanic orogen Gondwanan orogen Tabarin orogen Orógeno Oclóyico Orógeno Famatiniano Orógeno Chánico Orógeno Gondwánico Orógeno Tabarin |
| topic |
Geología Ocloyic orogen Famatinian orogen Chanic orogen Gondwanan orogen Tabarin orogen Orógeno Oclóyico Orógeno Famatiniano Orógeno Chánico Orógeno Gondwánico Orógeno Tabarin |
| dc.description.none.fl_txt_mv |
During the late Neoproterozoic and Paleozoic, the Argentinean-Chilean Andes and, since the late Paleozoic, the Antarctic Peninsula formed part of the southwestern margin of Gondwana. During this long period of the geological time, a set of continetal fragments of variable size and allochtonie was successively accreted to that margin. This process, coupled with the development of several subductive systems, resulted in six Paleozoic orogenies, which have different temporal and spatial extensions: Pampean (Neoproterozoic-early Cambrian), Famatinian (Middle Ordovician- Silurian), Ocloyic (Middle Ordovician-Devonian), Chanic (Middle Devonian-early Carboniferous), Gondwanan (Middle Devonian-middle Permian) and Tabarin (late Permian-Triassic). All these orogenies had a collisional character, with the exception of the Tabarin and a part of the Gondwanan orogenies that are subduction-related. Centro de Investigaciones Geológicas |
| description |
During the late Neoproterozoic and Paleozoic, the Argentinean-Chilean Andes and, since the late Paleozoic, the Antarctic Peninsula formed part of the southwestern margin of Gondwana. During this long period of the geological time, a set of continetal fragments of variable size and allochtonie was successively accreted to that margin. This process, coupled with the development of several subductive systems, resulted in six Paleozoic orogenies, which have different temporal and spatial extensions: Pampean (Neoproterozoic-early Cambrian), Famatinian (Middle Ordovician- Silurian), Ocloyic (Middle Ordovician-Devonian), Chanic (Middle Devonian-early Carboniferous), Gondwanan (Middle Devonian-middle Permian) and Tabarin (late Permian-Triassic). All these orogenies had a collisional character, with the exception of the Tabarin and a part of the Gondwanan orogenies that are subduction-related. |
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2017 |
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2017-08 |
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