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 …

In accretionary convergent margins, the subduction interface is formed by a lower plate
décollement above which sediments are scraped off and incorporated into the accretionary …

Basement inherited structures represent a significant factor affecting thrust propagation
dynamics during the growth of fold-and-thrust belts. In this study inspirited from seismic data …

Inverted structures provide traps for petroleum exploration, typically four-way structural
closures. As to the degree of inversion, based on a large number of worldwide examples …

Polyphase deformation of continental crust is analysed through physical analogue models
for settings wherein platform–basin geometries at passive continental margins are subject to …

We present a series of 2D thermo-mechanical numerical experiments of thick-skinned
crustal extension including a pre-rift salt horizon and subsequent thin-, thick-skinned, or …

Fold and thrust belt architecture may be influenced by basement geometry of the downgoing
plate. This influence is notoriously difficult to assess due to a common lack of subsurface …

In the rejuvenated mountain front, preexisting basement structures are often reactivated and
interact with the subsequent thin‐skinned deformation. How the deep structures affect the …

The inversion of passive margins and their transportation into fold-and-thrust belts is a
critical stage of mountain-building processes. In this study, we selected the Doldenhorn …

Abstract The External Dinarides fold-thrust belt formed during Mid-Eocene–Oligocene times
by SW-propagating thrusting from the Internal Dinarides towards the Adriatic foreland …