Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Carlos E. Gardini"'
Autor:
Carlos E. Gardini, Carlos H. Costa, Jason M. Cesta, Andres D. Richard, Lewis A. Owen, Jeremy M. Rimando, Lindsay M. Schoenbohm
Publikováno v:
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Most of the permanent deformation in the Pampean Flat slab segment of the central Andes is taken up at the Andean Orogenic Front in Argentina, a narrow zone between the Eastern Precordillera and Sierras Pampeanas that comprises one of the world's mos
Autor:
Carlos H. Costa, Didier Bourlès, Emilio A. Ahumada, Michel Sébrier, Lionel Siame, Olivier Bellier, Carlos E. Gardini, Hector Cisneros
Publikováno v:
Tectonics. 34:1129-1153
Quaternary tectonic and denudation rates are investigated for an actively growing basement anticline: the Sierra Pie de Palo range, which belongs to the Andean foreland of Northwestern Argentina (28°S–33°S). In this study, a detailed morphometric
Scarps related to Quaternary-active thrust splays propagating in alluvial bajadas of the Southern Precordillera of Argentina (32°20′) were studied through detailed topographic surveys, in order to understand the reliability of these landforms as d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::012e0839ca0d1e60a050e200d17a8e2e
https://www.sciencedirect.com/science/article/pii/S1040618216300404
https://www.sciencedirect.com/science/article/pii/S1040618216300404
Autor:
Carlos E. Gardini, Fabricio Rodrigo Vazquez, Emilio A. Ahumada, Carlos H. Costa, Hans Diederix
Publikováno v:
Geological Society, London, Special Publications. 399:245-266
Publikováno v:
Journal of Seismology. 5:399-409
Neogene strain from the subducting Nazca plate is widely distributed in theAndean foreland as a result of flat-lying subduction beneath central westernArgentina (28°–33°S latitude). This fact is indicated byuplifted basement blocks bounded by rev
Publikováno v:
Journal of South American Earth Sciences. 13:287-292
The Sierra de Las Penas-Las Higueras (Mendoza Province, Argentina, 32°15′S–32°45′S) presents one of the clearest and most continuous exposures of the Quaternary thrust front of the Precordilleran fold-and-thrust belt. It is characterized by a