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• W801530499 endingPage "529" @default.
• W801530499 startingPage "511" @default.
• W801530499 abstract "A broad range of processes acted simultaneously during the Quaternary producing relief in the Andes and adjacent foreland, from the Chilean coast, where the Pacific Ocean floor is being subducted beneath South American, to the Brazilian and the Argentinean Atlantic platform area. This picture shows to be complex and responds to a variety of processes. The Geoid exemplifies this spectrum of uplift mechanisms, since it reflects an important change at 35°S along the Andes and the foreland that could be indicating the presence of dynamic forces modeling the topography with varying intensity through the subduction margin. On the other hand, mountains uplifted in the Atlantic margin, along a vast sector of the Brazilian Atlantic coast and inland regions seem to be created at the area where the passive margin has been hyper-extended and consequently mechanically debilitated and the forearc region shifts eastwardly at a similar rate than the westward advancing continent. Therefore the forearc at the Arica latitudes can be considered as relatively stationary and dynamically sustained by a perpendicular-to-the-margin asthenospheric flow that inhibits trench roll back, determining a highly active orogenic setting at the eastern Andes in the Subandean region. To the south, the Pampean flat subduction zone creates particular conditions for deformation and rapid propagation of the orogenic front producing a high-amplitude orogen. In the southern Central and Patagonian Andes, mountain (orogenic) building processes are attenuated, becoming dominant other mechanisms of exhumation such as the i) impact of mantle plumes originated in the 660 km mantle transition, ii) the ice-masse retreat from the Andes after the Pleistocene producing an isostatic rebound, iii) the dynamic topography associated with the opening of an asthenospheric window during the subduction of the Chile ridge and slab tearing processes, iv) the subduction of oceanic swells linked to transform zones and v) the accretion of oceanic materials beneath the forearc region. Additionally and after last geodetic studies, vi) exhumation due to co- and post-seismic lithospheric stretching associated with large earthquakes along the subduction zone, also shows to be a factor associated with regional uplift that needs to be further considered as an additional mechanism from the Chilean coast to the western retroarc area. Finally, this revision constitutes a general picture about the different mechanisms of uplift and active deformation along the Southern Andes, in which orogenic processes become dominant north of 35°S, while south of these latitudes dynamic forces seem to predominate all over the Patagonian platform." @default.
• W801530499 created "2016-06-24" @default.
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• W801530499 date "2015-12-01" @default.
• W801530499 modified "2023-10-15" @default.
• W801530499 title "A review about the mechanisms associated with active deformation, regional uplift and subsidence in southern South America" @default.
• W801530499 cites W1488160313 @default.
• W801530499 cites W1532460077 @default.
• W801530499 cites W1539959491 @default.
• W801530499 cites W1569361708 @default.
• W801530499 cites W1576023586 @default.
• W801530499 cites W1608444353 @default.
• W801530499 cites W1610651606 @default.
• W801530499 cites W1624477729 @default.
• W801530499 cites W1627383688 @default.
• W801530499 cites W1644522513 @default.
• W801530499 cites W1840778637 @default.
• W801530499 cites W1876965659 @default.
• W801530499 cites W1907316404 @default.
• W801530499 cites W1949250275 @default.
• W801530499 cites W1969021187 @default.
• W801530499 cites W1969764787 @default.
• W801530499 cites W1971792457 @default.
• W801530499 cites W1972387084 @default.
• W801530499 cites W1973576637 @default.
• W801530499 cites W1976562750 @default.
• W801530499 cites W1981651301 @default.
• W801530499 cites W1982029293 @default.
• W801530499 cites W1985000995 @default.
• W801530499 cites W1987006553 @default.
• W801530499 cites W1987166327 @default.
• W801530499 cites W1993128170 @default.
• W801530499 cites W1993581436 @default.
• W801530499 cites W2002644910 @default.
• W801530499 cites W2002763218 @default.
• W801530499 cites W2003877865 @default.
• W801530499 cites W2007609987 @default.
• W801530499 cites W2008787240 @default.
• W801530499 cites W2016985841 @default.
• W801530499 cites W2017512729 @default.
• W801530499 cites W2020858340 @default.
• W801530499 cites W2023010288 @default.
• W801530499 cites W2027904321 @default.
• W801530499 cites W2029362687 @default.
• W801530499 cites W2033280630 @default.
• W801530499 cites W2035216517 @default.
• W801530499 cites W2035932728 @default.
• W801530499 cites W2041297773 @default.
• W801530499 cites W2047537000 @default.
• W801530499 cites W2054289340 @default.
• W801530499 cites W2055168533 @default.
• W801530499 cites W2056837513 @default.
• W801530499 cites W2057368297 @default.
• W801530499 cites W2064753511 @default.
• W801530499 cites W2065922875 @default.
• W801530499 cites W2067042055 @default.
• W801530499 cites W2070299474 @default.
• W801530499 cites W2074894847 @default.
• W801530499 cites W2076136278 @default.
• W801530499 cites W2076989802 @default.
• W801530499 cites W2079651423 @default.
• W801530499 cites W2081524475 @default.
• W801530499 cites W2083136661 @default.
• W801530499 cites W2084814623 @default.
• W801530499 cites W2087867658 @default.
• W801530499 cites W2089267415 @default.
• W801530499 cites W2089418151 @default.
• W801530499 cites W2105230405 @default.
• W801530499 cites W2110381646 @default.
• W801530499 cites W2112568224 @default.
• W801530499 cites W2113340888 @default.
• W801530499 cites W2113559163 @default.
• W801530499 cites W2116636746 @default.
• W801530499 cites W2118197212 @default.
• W801530499 cites W2119072040 @default.
• W801530499 cites W2123755966 @default.
• W801530499 cites W2126113995 @default.
• W801530499 cites W2129593546 @default.
• W801530499 cites W2134687993 @default.
• W801530499 cites W2136375113 @default.
• W801530499 cites W2154603570 @default.
• W801530499 cites W2161531362 @default.
• W801530499 cites W2162447099 @default.
• W801530499 cites W2165776961 @default.
• W801530499 cites W2168593275 @default.

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