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Geochemically, these magmas display an arc signature. More information or change your settings.

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Oops, something went wrong, please try again later. Tectonic activity started during the Late Oligocene and is documented by thrust and reverse faulting.

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Due to thick-skinned deformation, the former coherent part of the foreland basin was subdivided into broken-foreland basins filled with alluvial and eolian sediments Chacras Formation.

Cenozoic sedimentation started during the Late Eocene at the climax of the Incaic phase in the Chilean Precordillera.

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During the Pliocene, tectonic shortening continued with local strike-slip components. Can you please check? Those prices don't take into account any promotion and are VAT included. La Fourchette SAS and the restaurant, being data controllers, process personal data for the purposes of reservation processing and customer relations.

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These relief-forming processes reduced the Salar de Antofalla basin to its present narrow and elongated shape and triggered the final alluvial fan sedimentation Escondida Formation. This e-mail address seems incorrect.

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My email You have succesfully subscribed to the newsletter! They were generated by interaction of basaltic magmas with the Andean continental crust thickened to at least 40 km. Reverse faulting and thrusting during the Middle to Late Miocene led to an intra-arc basin filled with thick alluvial fan and evaporite sediments Juncalito Formation.

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Your loyalty is rewarded! Several intermediate stratovolcanic centers began to erupt between 18 Ma and 14 Ma.

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Their buildup could have been accompanied with initial uplift and crustal thickening of the Southern Puna. As a consequence of continuing contractional tectonism during Early Miocene, the Salar de Antofalla area was further subdivided into a number of small intra-arc depocenters in which alluvial fan and fluvial sediments Potrero Grande Formation were deposited.

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