The Relation Between Neogene Denudation of the Southernmost Andes and Sedimentation in the Offshore Argentine and Malvinas Basins During the Opening of the Drake Passage

GHIGLIONE, MATÍAS; SUE, CHRISTIAN; RAMOS MIGUEL ESTEBAN; TOBAL, JONATHAN; GALLARDO, ROCÍO E.

CONCEPCIÓN

Congreso; XV CONGRESO GEOLÓGICO CHILENO 2018 UNIVERSIDAD DE CONCEPCIÓN - CHILE; 2018

UNIVERSIDAD DE CONCEPCIÓN-CHILE

Abstract The Neogene orogenic growth of the Southern Patagonian Andes has been related to the approximation and collision of aseries of segments of the Chile seismic ridge, which separates the Antarctic and Nazca plates, against South America. The compiledthermochronological data consistently indicates an eastward moving trend of exhumation, were uplift of the western basement domainoccurred from 34 to 15 Ma and was followed by denudation of the basement front and the fold and thrust belt between 20 and 5 Ma.There has been an assumption that tectonic growth in southern Patagonia ended in late Miocene times, largely based on the top age ofthe molasse deposits of the Santa Cruz Formation, spanning from 22?19 to 14 Ma. There is, however, multiple thermochronologicalevidence that exhumation in the hinterland continued profusely, with large volumes of rock denudated rapidly between 15 and 5 Ma,and steadily since 7 Ma. However, continental sedimentation rate was very low in the Magallanes?Austral Basin of the SouthernmostAndes after 14 Ma, an effect produced by the dynamic uplift of Patagonia. Contrastingly, the upper Miocene?lower Plioceneconstitutes an aggradational period very well developed in the offshore Argentine continental margin. We propose that the greatvolumes of sediments produced by Miocene?Pliocene denudation of the Southernmost Andes bypassed Patagonia and reached theArgentina and Malvinas basins, where they were accommodated in thick sequences with high sedimentation rates. Thosesediments were distributed along the Southern Atlantic margin by sub-Antarctic currents, which propagated into the Argentinecontinental margin during the deepening of the Drake Passage. The sediments were probably funneled through gargantuan fluvialand glacifluvial W?E systems, similar to those preserved in Patagonia from the last glaciation, and axially through the FuegianAndes foothills toward the offshore basins.