0000000000724995

AUTHOR

Miguel E. Ramos

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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Seismotectonic implications of the south chile ridge subduction beneath the patagonian andes

2021

International audience; The South Chile ridge (SCR) intersects the Patagonian trench around 46° 09’S, forming the triple junction among the Antarctic, Nazca, and South America plates. Subduction of the SCR since ~18 Ma produced the opening of a slab window beneath Patagonia and a noticeable magmatic gap in the cordillera, profuse volcanism, and topographic uplift in the retroarc. To study seismicity distribution and present‐day stress resulting from this particular framework, we analyze databases of seismic events and earthquake focal mechanisms. Our study finds that clusters of intraplate crustal seismic events are disrupted by a ~450‐470 km seismicity gap above the slab window. Calculated…

[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics010504 meteorology & atmospheric sciencesSubductionRidge (meteorology)Geology010502 geochemistry & geophysics01 natural sciencesArchaeologyGeology0105 earth and related environmental sciences
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