Basin inversion involves the reversal of subsidence in a basin due to compressional tectonic
forces, leading to uplift of the basin's sedimentary infill. A thorough understanding of basin …

The orogenic growth of the Domeyko Cordillera was induced by a positive tectonic
inversion. In this work, we have validated this interpretation from new field data, which were …

The presence of pre-existing rheological heterogeneities in the lithosphere plays a
significant role during subsequent stages of deformation in essentially every geological …

Analogue models are often used to model long-term geological processes such as mountain
building or basin inversion. Most of these models use granular materials such as sand or …

This study aims to explain the selective reactivation of normal faults during the Andean
orogeny at the Southern Central Andes western flank. We conducted a structural mapping …

Andean fold-and-thrust belts (FTBs) in the western border of South America show important
along-strike variations in their structural style (thin-or thick-skinned) and shortening …

In this work, we present an update for the conceptual model of the El Tatio-La Torta
geothermal system, one of the most studied geothermal fields in the Central Andes of South …

Basin inversion is a process that takes place when a sedimentary basin is subjected to
compressional stresses resulting in the reactivation of pre-existing faults and/or the …

Abstract The late Eocene-Early Miocene intra-arc Abanico extensional basin represents a
major feature in central Chile (∼ 31°-42° S). Such basin system concentrated the magmatic …

Basin inversion is a process that takes place when a sedimentary basin is subjected to
compressional stresses and may result in the reactivation of pre-existing faults and/or the …