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César Navarrete

Researcher at National University of Patagonia San Juan Bosco

Publications -  24
Citations -  540

César Navarrete is an academic researcher from National University of Patagonia San Juan Bosco. The author has contributed to research in topics: Subduction & Cretaceous. The author has an hindex of 12, co-authored 23 publications receiving 422 citations.

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Patagonian broken foreland and related synorogenic rifting: The origin of the Chubut Group Basin

TL;DR: In this paper, structural, 2D and 3D seismic data at the San Bernardo FTB and the adjacent Rio Mayo Basin were analyzed to unravel the different evolutionary stages of the Chubut Group Basin.
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Triassic to Middle Jurassic geodynamic evolution of southwestern Gondwana: From a large flat-slab to mantle plume suction in a rollback subduction setting

TL;DR: A geodynamic evolution model of the southwestern region of Gondwana from the late Triassic to the middle Jurassic period is proposed in this paper, based on new data collected in the Patagonian region and an exhaustive bibliographic review.
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A geodynamic model linking Cretaceous orogeny, arc migration, foreland dynamic subsidence and marine ingression in southern South America

TL;DR: In this paper, the authors synthesize the tectonomagmatic evolution of the Andes between 35°30′S to 48°S with the aim to spotlight early contractional phases on Andean orogenic building and to analyze their potential driving processes.
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Cenomanian-? early Turonian minimum age of the Chubut Group, Argentina: SHRIMP U-Pb geochronology

TL;DR: In this paper, four new SHRIMP U-Pb zircon ages older than 93 Ma from samples of the two uppermost formations accumulated in two different depocenters (Golfo de San Jorge and Canadon Asfalto basins) of the Chubut Group in central Argentinean Patagonia, establish a prelate Cenomanian-? early Turonian age for the group.
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Tectonic inversion events in the western San Jorge Gulf Basin from seismic, borehole and field data

TL;DR: In this paper, the authors analyzed subsurface information (2D and 3D seismic lines and oil wells) located in the western area of the basin and compared this with surface data of the southern Bernardides System.