Evolución Geodinámica de los Andes argentino-chilenos y la Península Antártica durante el Neoproterozoico tardío y el Paleozoico

N. Heredia, J. García-Sansegundo, G. Gallastegui, P. Farias, R. Giacosa, J. L. Alonso, P. Busquets, R. Charrier, P. Clariana, F. Colombo, A. Cuesta, J. Gallastegui, L. Giambiagi, L. González-Menéndez, C. O. Limarino, F. Martín-González, I. Méndez-Bedia, D. Pedreira, L. Quintana, L. R. Rodríguez-FernándezA. Rubio-Ordóñez, R. Seggiaro, S. Serra-Varela, L. Spalletti, R. Cardó, V. A. Ramos

Resultado de la investigación: Article

5 Citas (Scopus)

Resumen

During the late Neoproterozoic and Paleozoic times, the Argentine-Chilean Andes, -and since the late Paleozoic the Antarctic Peninsula,- formed part of the southwestern margin of Gondwana. During this period of time, several continental fragments of variable extension and allochtonie were successively accreted to that margin, resulted in six Paleozoic orogenies of different temporal and spatial extension: Pampean (Ediacaran-early Cambrian), Famatinian (Middle Ordovician-Silurian), Chanic (Middle Devonian-early Carboniferous), Ocloyic (Middle Ordovician-Devonian), Gondwanan (Middle Devonian-middle Permian) and Tabarin (late Permian-Triassic). All these orogenies had a collisional character, with the exception of the Tabarin and the Gondwanan south of 38ºS.

Idioma originalSpanish
Páginas (desde-hasta)237-278
Número de páginas42
PublicaciónTrabajos de Geologia
N.º36
DOI
EstadoPublished - 1 ene 2016

Huella dactilar

geodynamics
Paleozoic
Ordovician
Permian
Ediacaran
Gondwana
Silurian
Triassic

ASJC Scopus subject areas

  • Geology

Citar esto

Heredia, N., García-Sansegundo, J., Gallastegui, G., Farias, P., Giacosa, R., Alonso, J. L., ... Ramos, V. A. (2016). Evolución Geodinámica de los Andes argentino-chilenos y la Península Antártica durante el Neoproterozoico tardío y el Paleozoico. Trabajos de Geologia, (36), 237-278. https://doi.org/10.17811/tdg.36.2016.237-278
Heredia, N. ; García-Sansegundo, J. ; Gallastegui, G. ; Farias, P. ; Giacosa, R. ; Alonso, J. L. ; Busquets, P. ; Charrier, R. ; Clariana, P. ; Colombo, F. ; Cuesta, A. ; Gallastegui, J. ; Giambiagi, L. ; González-Menéndez, L. ; Limarino, C. O. ; Martín-González, F. ; Méndez-Bedia, I. ; Pedreira, D. ; Quintana, L. ; Rodríguez-Fernández, L. R. ; Rubio-Ordóñez, A. ; Seggiaro, R. ; Serra-Varela, S. ; Spalletti, L. ; Cardó, R. ; Ramos, V. A. / Evolución Geodinámica de los Andes argentino-chilenos y la Península Antártica durante el Neoproterozoico tardío y el Paleozoico. En: Trabajos de Geologia. 2016 ; N.º 36. pp. 237-278.
@article{86ac8107eb8d4a15abc18cfabff4c55a,
title = "Evoluci{\'o}n Geodin{\'a}mica de los Andes argentino-chilenos y la Pen{\'i}nsula Ant{\'a}rtica durante el Neoproterozoico tard{\'i}o y el Paleozoico",
abstract = "During the late Neoproterozoic and Paleozoic times, the Argentine-Chilean Andes, -and since the late Paleozoic the Antarctic Peninsula,- formed part of the southwestern margin of Gondwana. During this period of time, several continental fragments of variable extension and allochtonie were successively accreted to that margin, resulted in six Paleozoic orogenies of different temporal and spatial extension: Pampean (Ediacaran-early Cambrian), Famatinian (Middle Ordovician-Silurian), Chanic (Middle Devonian-early Carboniferous), Ocloyic (Middle Ordovician-Devonian), Gondwanan (Middle Devonian-middle Permian) and Tabarin (late Permian-Triassic). All these orogenies had a collisional character, with the exception of the Tabarin and the Gondwanan south of 38ºS.",
keywords = "Antarctic Peninsula, Argentine-Chilean Andes, Chanic orogen, Famatinian orogen, Geodynamic evolution, Gondwanan orogen, Ocloyic orogen, Paleozoic, Tabarin orogen",
author = "N. Heredia and J. Garc{\'i}a-Sansegundo and G. Gallastegui and P. Farias and R. Giacosa and Alonso, {J. L.} and P. Busquets and R. Charrier and P. Clariana and F. Colombo and A. Cuesta and J. Gallastegui and L. Giambiagi and L. Gonz{\'a}lez-Men{\'e}ndez and Limarino, {C. O.} and F. Mart{\'i}n-Gonz{\'a}lez and I. M{\'e}ndez-Bedia and D. Pedreira and L. Quintana and Rodr{\'i}guez-Fern{\'a}ndez, {L. R.} and A. Rubio-Ord{\'o}{\~n}ez and R. Seggiaro and S. Serra-Varela and L. Spalletti and R. Card{\'o} and Ramos, {V. A.}",
year = "2016",
month = "1",
day = "1",
doi = "10.17811/tdg.36.2016.237-278",
language = "Spanish",
pages = "237--278",
journal = "Trabajos de Geologia",
issn = "0474-9588",
publisher = "Universidad de Oviedo",
number = "36",

}

Heredia, N, García-Sansegundo, J, Gallastegui, G, Farias, P, Giacosa, R, Alonso, JL, Busquets, P, Charrier, R, Clariana, P, Colombo, F, Cuesta, A, Gallastegui, J, Giambiagi, L, González-Menéndez, L, Limarino, CO, Martín-González, F, Méndez-Bedia, I, Pedreira, D, Quintana, L, Rodríguez-Fernández, LR, Rubio-Ordóñez, A, Seggiaro, R, Serra-Varela, S, Spalletti, L, Cardó, R & Ramos, VA 2016, 'Evolución Geodinámica de los Andes argentino-chilenos y la Península Antártica durante el Neoproterozoico tardío y el Paleozoico', Trabajos de Geologia, n.º 36, pp. 237-278. https://doi.org/10.17811/tdg.36.2016.237-278

Evolución Geodinámica de los Andes argentino-chilenos y la Península Antártica durante el Neoproterozoico tardío y el Paleozoico. / Heredia, N.; García-Sansegundo, J.; Gallastegui, G.; Farias, P.; Giacosa, R.; Alonso, J. L.; Busquets, P.; Charrier, R.; Clariana, P.; Colombo, F.; Cuesta, A.; Gallastegui, J.; Giambiagi, L.; González-Menéndez, L.; Limarino, C. O.; Martín-González, F.; Méndez-Bedia, I.; Pedreira, D.; Quintana, L.; Rodríguez-Fernández, L. R.; Rubio-Ordóñez, A.; Seggiaro, R.; Serra-Varela, S.; Spalletti, L.; Cardó, R.; Ramos, V. A.

En: Trabajos de Geologia, N.º 36, 01.01.2016, p. 237-278.

Resultado de la investigación: Article

TY - JOUR

T1 - Evolución Geodinámica de los Andes argentino-chilenos y la Península Antártica durante el Neoproterozoico tardío y el Paleozoico

AU - Heredia, N.

AU - García-Sansegundo, J.

AU - Gallastegui, G.

AU - Farias, P.

AU - Giacosa, R.

AU - Alonso, J. L.

AU - Busquets, P.

AU - Charrier, R.

AU - Clariana, P.

AU - Colombo, F.

AU - Cuesta, A.

AU - Gallastegui, J.

AU - Giambiagi, L.

AU - González-Menéndez, L.

AU - Limarino, C. O.

AU - Martín-González, F.

AU - Méndez-Bedia, I.

AU - Pedreira, D.

AU - Quintana, L.

AU - Rodríguez-Fernández, L. R.

AU - Rubio-Ordóñez, A.

AU - Seggiaro, R.

AU - Serra-Varela, S.

AU - Spalletti, L.

AU - Cardó, R.

AU - Ramos, V. A.

PY - 2016/1/1

Y1 - 2016/1/1

N2 - During the late Neoproterozoic and Paleozoic times, the Argentine-Chilean Andes, -and since the late Paleozoic the Antarctic Peninsula,- formed part of the southwestern margin of Gondwana. During this period of time, several continental fragments of variable extension and allochtonie were successively accreted to that margin, resulted in six Paleozoic orogenies of different temporal and spatial extension: Pampean (Ediacaran-early Cambrian), Famatinian (Middle Ordovician-Silurian), Chanic (Middle Devonian-early Carboniferous), Ocloyic (Middle Ordovician-Devonian), Gondwanan (Middle Devonian-middle Permian) and Tabarin (late Permian-Triassic). All these orogenies had a collisional character, with the exception of the Tabarin and the Gondwanan south of 38ºS.

AB - During the late Neoproterozoic and Paleozoic times, the Argentine-Chilean Andes, -and since the late Paleozoic the Antarctic Peninsula,- formed part of the southwestern margin of Gondwana. During this period of time, several continental fragments of variable extension and allochtonie were successively accreted to that margin, resulted in six Paleozoic orogenies of different temporal and spatial extension: Pampean (Ediacaran-early Cambrian), Famatinian (Middle Ordovician-Silurian), Chanic (Middle Devonian-early Carboniferous), Ocloyic (Middle Ordovician-Devonian), Gondwanan (Middle Devonian-middle Permian) and Tabarin (late Permian-Triassic). All these orogenies had a collisional character, with the exception of the Tabarin and the Gondwanan south of 38ºS.

KW - Antarctic Peninsula

KW - Argentine-Chilean Andes

KW - Chanic orogen

KW - Famatinian orogen

KW - Geodynamic evolution

KW - Gondwanan orogen

KW - Ocloyic orogen

KW - Paleozoic

KW - Tabarin orogen

UR - http://www.scopus.com/inward/record.url?scp=85061617722&partnerID=8YFLogxK

U2 - 10.17811/tdg.36.2016.237-278

DO - 10.17811/tdg.36.2016.237-278

M3 - Article

AN - SCOPUS:85061617722

SP - 237

EP - 278

JO - Trabajos de Geologia

JF - Trabajos de Geologia

SN - 0474-9588

IS - 36

ER -