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 …

This work includes, first, a synthesis of experimental analogue modelling programs
assessing the influence of along-strike thickness variations in the development of oblique …

The Basque-Cantabrian junction corresponds to an inverted rift accommodation zone at the
limit between the former hyperextended Pyrenean and Cantabrian rift segments. The …

Abstract The Western Domain of the Magallanes Fold-and-Thrust Belt (MFTB) between 52°-
54° S is part of a poorly studied hinterland region of the southernmost Andean Cordillera …

Resolving the role of longitudinal versus transverse sediment dispersal in ancient
sedimentary basins is paramount for understanding filling history and the timing of source …

Abstract The Cretaceous-Cenozoic evolution of the Southern Patagonian Andes is one of
the most prominent examples of coupling between subduction processes and climatic …

We present field and seismic evidence for the existence of C oniacian–C ampanian
syntectonic angular unconformities within basal foreland basin sequences of the A ustral or …

A key event in the paleogeographic evolution of the Austral-Magallanes foreland basin was
the Santonian–Maastrichtian continentalization, marked by the appearance of deltaic, fluvial …

Abstract The Southern Patagonian Andes at the latitude of the Chile Triple junction in
Argentina and Chile (46°–47.5° S) are the object of an ongoing discussion regarding their …

We present a multidisciplinary study in the Austral-Magallanes basin combining U-Pb
geochronology and provenance analysis with structural modelling to unravel the evolution of …