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Politics, Citizenship and Rightsons predicting the collision of the Antarctic Peninsula against the Fuegian Andes due to accelerated convergence rates. Afterward, three phases of Cenozoic deformation in the southernmost Andes that can also be tied to tectonics of the Scotia Arc occurred: (1) a Paleocene–early Eocene continental st

Gleason-score

,Changes in Source Areas at Neuquén Basin: Mesozoic Evolution and Tectonic Setting Based on U–Pb Agel fall or by a period of exhumation of the Sierras Pampeanas basement linked to generation of rift systems. The source regions in the Late Cretaceous (foreland stage) indicate an uplift of a mountain chain and exhumation along the Andean magmatic arc; although younger and distal units showed that a

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,Progression of the Deformation in the Southern Central Andes (37°S),the activity of neotectonic structures during landscape evolution. As a result, an evolutionary model is presented for the Southern Central Andes in which four pulses of deformation were recognized in agreement with previous proposals, although with a variable distribution reflecting a complex patte

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,Cenozoic Deformational Processes in the North Patagonian Andes Between 40° and 43°S,ers were formed toward the foreland. Additionally, eastward shifting of Miocene calc-alkaline arc rocks occurred at these latitudes, which is interpreted as indicative of a significant change in the subduction parameters at this time. Deep crustal retroarc structure is evaluated through inversion of

Goblet-Cells

The North Patagonian Orogen: Meso-Cenozoic Evolution from the Andes to the Foreland Area,ion is documented at the retroarc zone. At this moment, a series of mid-ocean ridges collided one after another against the Patagonian margin. A causative relation between young lithosphere subduction, slab shallowing, orogenesis and eruption of mafic magmatism at the arc and retroarc region has bee

Cubicle

,Growth of the Southern Patagonian Andes (46–53°S) and Their Relation to Subduction Processes, the Coniacian–Santonian exhumation of the Sarmiento Ophiolitic Complex and propagation of the orogenic front toward the foreland. The second cycle, during Paleogene deformation, coincided with an Eocene volcanic arc gap, and seems to be related to the Fallarón-Phoenix seismic ridge collision. The r

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,Orogenic Growth of the Fuegian Andes (52–56°) and Their Relation to Tectonics of the Scotia Arc,ons predicting the collision of the Antarctic Peninsula against the Fuegian Andes due to accelerated convergence rates. Afterward, three phases of Cenozoic deformation in the southernmost Andes that can also be tied to tectonics of the Scotia Arc occurred: (1) a Paleocene–early Eocene continental st

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The Weaponization of Congressional Oversightt area, separated from the arc front zone. Computed elastic thicknesses from gravity data show a good correlation with these areas with abnormal heat flow associated with retroarc stretching and magmatic emplacement in the last 5–2 Ma.

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,Tectonic Evolution of the Northern Patagonian Andes (40°S),t area, separated from the arc front zone. Computed elastic thicknesses from gravity data show a good correlation with these areas with abnormal heat flow associated with retroarc stretching and magmatic emplacement in the last 5–2 Ma.