The Pre-Andean Phases of Construction of the Southern Andes Basement in Neoproterozoic–Paleozoic Times

Autor: Nemesio Heredia, P. Farias, D. Pedreira, José María Tubía, Raúl Eduardo Giacosa, Fidel Martín-González, Reynaldo Charrier, Ferran Colombo, Luis Roberto Rodríguez-Fernández, Victor A. Ramos, Gloria Gallastegui, Álvaro Rubio-Ordóñez, Samanta Serra-Varela, A. Cuesta, Luis González-Menéndez, Luis Quintana, Pilar Clariana, Oscar Limarino, Luis Antonio Spalletti, Pere Busquets, Raúl E. Seggiaro, J. Gallastegui, Fernando Hongn, Laura Giambiagi, Raúl Cardó, Juan Juis Alonso, Joaquín García-Sansegundo

Publikováno v: The Evolution of the Chilean-Argentinean Andes ISBN: 9783319677736
The Evolution of the Chilean-Argentinean Andes
RID-UNRN (UNRN)
Universidad Nacional de Río Negro
instacron:UNRN

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 allochto

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::23c192734ef4db801c4f5a04347a6e47
https://doi.org/10.1007/978-3-319-67774-3_5

Late Palaeozoic lithostratigraphy of the Andean Precordillera revisited (San Juan Province, Argentina)

Autor: Raúl Cardó, Pere Busquets, Nemesio Heredia, Luis Antonio Spalletti, I. Méndez-Bedia, F. Colombo, Carlos Oscar Limarino

Publikováno v: SEDICI (UNLP)
Universidad Nacional de La Plata
instacron:UNLP
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET

New data on some neopalaeozoic lithostratigraphic units of the central sector of the Argentinean Precordillera are presented. The western Precordillera displays occasional outcrops of siliciclastic rocks of the Late Palaeozoic. These rocks are separa

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::890802c4656ff76fd1e18edeb1e2720f
https://doi.org/10.5209/rev_jige.2014.v40.n2.45311

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