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The Pre-Andean Phases of Construction of the Southern Andes Basement in Neoproterozoic–Paleozoic Times
dc.contributor.author | Heredia Carballo, Nemesio | |
dc.contributor.author | García-Sansegundo, Joaquín | |
dc.contributor.author | Gallastegui Suárez, Gloria | |
dc.contributor.author | Farias Arquer, Pedro José | |
dc.contributor.author | Giocasa, Raúl | |
dc.contributor.author | Hongn, Fernando | |
dc.contributor.author | Tubía, José María | |
dc.contributor.author | Alonso Alonso, Juan Luis | |
dc.contributor.author | Busquets, Pere | |
dc.contributor.author | Charrier, Reynaldo | |
dc.contributor.author | Clariana, Pilar | |
dc.contributor.author | Colombo, Ferrán | |
dc.contributor.author | Cuesta Fernández, Andrés | |
dc.contributor.author | Gallastegui Suárez, Jorge | |
dc.contributor.author | Giambiagi, Laura | |
dc.date.accessioned | 2018-05-03T12:05:19Z | |
dc.date.available | 2018-05-03T12:05:19Z | |
dc.date.issued | 2018 | |
dc.identifier.citation | Heredia N. et al. (2018) The Pre-Andean Phases of Construction of the Southern Andes Basement in Neoproterozoic–Paleozoic Times. In: Folguera A. et al. (eds) The Evolution of the Chilean-Argentinean Andes. Springer Earth System Sciences. Springer, Cham; doi:10.1007/978-3-319-67774-3_5 | |
dc.identifier.isbn | 978-3-319-67774-3 | |
dc.identifier.isbn | 978-3-319-67773-6 | |
dc.identifier.uri | http://hdl.handle.net/10651/46858 | |
dc.description.abstract | During the late Neoproterozoic and Paleozoic times, the Southern Andes of Argentina and Chile (21º-55º S) formed part of the southwestern margin of Gondwana. During this period of time, a set of continental fragments of variable extent and allochtony was successively accreted to that margin, resulting in six Paleozoic orogenies of different temporal and spatial extension: Pampean (Ediacaran-early Cambrian), Famatinian (Early Ordovician-Silurian), Ocloyic (Middle Ordovician-Devonian), Chanic (Middle Devonian-early Carboniferous), Gondwanan (Middle Devonian-middle Permian) and Tabarin (late Permian-Triassic). All these orogenies culminate with collisional events, with the exception of the Tabarin and a part of the Gondwanan orogenies that are subduction-related. | eng |
dc.description.sponsorship | This chapter shows the main results of the InverAndes (BTE2002-04316-C03), PaleoAndes I (CGL2006-12415-CO3/BTE), PaleoAndes II (CGL2009-13706-CO3), TORANDES (CGL2012-38396-C03) projects, supported by the I+D+i Spanish Plan and FEDER Funds from the European Union | eng |
dc.description.statementofresponsibility | (et al.) | |
dc.format.extent | p. 111-131 | spa |
dc.language.iso | eng | spa |
dc.publisher | Springer | spa |
dc.relation.ispartof | The Evolution of the Chilean-Argentinean Andes | eng |
dc.rights | © Springer International Publishing AG, 2018 | |
dc.title | The Pre-Andean Phases of Construction of the Southern Andes Basement in Neoproterozoic–Paleozoic Times | eng |
dc.type | book part | spa |
dc.identifier.doi | 10.1007/978-3-319-67774-3_5 | |
dc.relation.projectID | BTE2002-04316-C03 | spa |
dc.relation.projectID | CGL2006-12415-CO3/BTE | |
dc.relation.projectID | TORANDES (CGL2012-38396-C03) | |
dc.relation.projectID | CGL2009-13706-CO3 | |
dc.relation.publisherversion | https://doi.org/10.1007/978-3-319-67774-3_5 | spa |
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