Miocene volcaniclastic foreland basin infill next to the exhumed north patagonian andean batholith: a record of collapse-caldera eruptions?

• Main Authors: López, Manuel, Bucher, Joaquin, García, Micaela Romina, D'Elia, Leandro, Bilmes, Andrés, Franzese, Juan Rafael
• Other Authors: Riller, Ullrich, Göllner, Paul
• Format: Journal/Newspaper
• Language: English
• Published: Schriften GeoUnion Alfred Wegener-Stiftung
• Subjects: TECTONICS; PATAGONIAN BROKEN FORELAND; COLLON CURA; https://purl.org/becyt/ford/1.5; https://purl.org/becyt/ford/1; antartic*
• Online Access: http://hdl.handle.net/11336/204538

The nature of Andean magmatism and their tectonic regimes results from variations in the angle of subduction of the Nazca and Antartic oceanic plates beneath South American plate. For the Patagonian Andes, a flat slab type subduction was proposed to the middle Miocene and the Patagonian Broken Foreland system was defined. At one time, foreland basins were filled with tens of primary and resedimented volcaniclastic materials that were distributed for more than 30.000 km2. In order to understand the relationship between tectonics and magmatic?volcanic feeder system interactions, we analysis the Miocene volcaniclastic infill succession of a basin located next to the exhumed Andean Batholith: the Collón Cura basin.The Collón Cura basin was mainly configured between 16 and 14.4 Ma due to the uplift of the north Patagonian Andes towards the west and the Sañicó Massif towards the east, evidencing the onset of the Patagonian Broken Foreland system. The uplift of the Patagonian Andes continues up to 4.8Ma. At the same time, a volcaniclastic succession of tuffs, lapilli tuffs and tuffaceous sandstones were deposited into the basin with up to 150 m-thick that reach an estimated volume of ~1800 km3. The succession is limited below by an angular unconformity and above by a regional erosional unconformity. Internally, the succession is characterized by three sections. The lower and upper sections are composed of ~50 - 70 m-thick of massive to roughly stratified and moderate-sorted vitric-rich lapilli tuff and tuffaceous sandstones. The middle section is characterized by 10 to 30 m thick of lenticular beds composed of massive, vitric-rich and moderately sorted lapilli-tuffs. Preliminary geochronological and magnetostratigraphic analysis constrain the volcaniclastic succession between 15.160 and 12.049 Ma and reveals that the whole succession has a normal polarity paleopole dated between 15.160 and 15.032 Ma, determining a maximum depositional time process of 128.000 years. Nevertheless, sedimentological features of the ...