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Meso-Cenozoic tectonics of the southern Patagonian foreland: Structural evolution and implications for Au–Ag veins in the eastern Deseado Region (Santa Cruz, Argentina)

Autor: Giacosa, R., Zubia, M., Sánchez, M., Allard, J.

Publikováno v: In Journal of South American Earth Sciences 2010 30(3):134-150

Structure of the Southern Patagonian Andes at 49ºS, Argentina

Autor: Giacosa, R., Fracchia, D., Heredia, N., Universidad Nacional de la Patagonia. Departamento de Geología

Publikováno v: Dipòsit Digital de Documents de la UAB
Universitat Autònoma de Barcelona
Recercat. Dipósit de la Recerca de Catalunya
instname
Recercat: Dipósit de la Recerca de Catalunya
Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)

This paper describes Late Paleozoic Gondwanan and Late Cretaceous to Early Cenozoic Andean structures in the Southern Patagonian Andes and an associated Extra-Andean region between lakes San Martín and Viedma. The study area encompasses a 200-km-lon

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::c3a586d346b4bd19450d5db265d5bd9a
https://ddd.uab.cat/record/99651

Una metodologia per la qualificazione del progetto edilizio,nell'ambito della normativa ISO 9001-2000 e del knowledge management

Autor: Lucat, Maurizio, Giacosa, R, Mantovani, Silvia, Revigliono, A.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______2153::cf9bef5b42ef60bd273d857a06fc9c58
http://hdl.handle.net/11583/1578393

La cuenca de antepais terciaria asociada a la faja plegada y corrida de los Andes Patagónicos entre los 41º y 42º S, SO de Argentina

Autor: GIACOSA, R., HEREDIA, N.

Publikováno v: Acta Geologica Hispanica; Vol.: 32 Núm.: 1-2; 103-112
RCUB. Revistas Científicas de la Universidad de Barcelona
instname
Acta geológica hispánica; 1997: Vol.: 32 Núm.: 1-2; p. 103-112

In Argentina, between 41"-42" S and related to the Andean Patagonian fold and thrust belt, two synorogenic sedimentary sequences were deposited in the Tertiary foreland basin. They represent different moments of the eastward migration of the orogenic

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::244730fb6d514a110916fa52e99cdce4
https://revistes.ub.edu/index.php/ActaGeologica/article/view/4602