0000000000724996

AUTHOR

Gonzalo Ronda

showing 2 related works from this author

Tectonic evolution of the northern Austral-Magallanes basin in the Southern Patagonian Andes from provenance analysis

2019

We studied the northern tip of the Austral-Magallanes basin in the Southern Patagonian Andes, between the Buenos Aires Lake and the Mayer River at 46°35′ SL and 48°35′ SL, respectively. Proposed objectives were: i) to differentiate Mesozoic-Cenozoic tectonostratigraphic units and, ii) to characterize the different deformational events that took place in the area linked to a variable regional geodynamic context. Sandstones provenance analysis was performed on the Aptian - Albian compressive retroarc deposits and Cenozoic foreland deposits. Studied samples were classified using tectonic discrimination diagrams which show: i) for Cretaceous rocks a dominant sediment source from a recycled orog…

010506 paleontologyProvenanceAptian010502 geochemistry & geophysics01 natural sciencesUnconformityCiencias de la Tierra y relacionadas con el Medio Ambiente//purl.org/becyt/ford/1 [https]//purl.org/becyt/ford/1.5 [https]PaleontologyGeologíaForeland basin0105 earth and related environmental sciencesEarth-Surface ProcessesRiftTECTONOSTRATIGRAPHIC UNITSGEODYNAMICSGeologySOUTHERN PATAGONIAN ANDESCretaceousBack-arc basinPROVENANCE ANALYSISCenomanianSEDIMENTARY PETROGRAPHYGeologyCIENCIAS NATURALES Y EXACTAS
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Late Cenozoic brittle deformation in the Southern Patagonian Andes: Record of plate coupling/decoupling during variable subduction?

2018

The Andes of southern Patagonia experienced a Miocene shift towards faster and higher angle subduction followed by the approach and collision of the Chile oceanic ridge. We present a kinematic study characterizing palaeostress fields computed from brittle tectonics to better constrain upper crustal deformation during this complex scenario. Although previous studies already suggested variable kinematics, it is striking that in a long-lasting subduction environment, the computed palaeostress tensors are mostly strike-slip (55%), while 35% are extensional, and only 10% compressive which are concentrated along a main frontal thrust. Cross-cutting relationships and synsedimentary deformation ind…

TECTONICS010504 meteorology & atmospheric sciencesPlate coupling/decouplingSouthern andesBrittle deformationGeodynamics010502 geochemistry & geophysics01 natural sciencesCiencias de la Tierra y relacionadas con el Medio Ambiente//purl.org/becyt/ford/1 [https]//purl.org/becyt/ford/1.5 [https]PLATE COUPLING/DECOUPLINGPatagoniaBRITTLE DEFORMATIONGeologíaComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsSOUTHERN ANDESSubductionTectonicsGEODYNAMICSGeologyPATAGONIACenozoicHumanitiesGeologyCIENCIAS NATURALES Y EXACTAS
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