West verging thrusts, synthetic with the Nazca‐South America subduction interface, have
been recently discovered at the western front of the Andes. At~ 33° 30′ S, the active San …

Sea‐floor topography of deep‐water folds is widely considered to have a major impact on
turbidity currents and their depositional systems, but understanding the flow response to …

Abstract Creating three-dimensional (3D) models to replicate geological structures is crucial
in discerning the geometry and kinematics of an orogen. The Jabal Hafit anticline, in the …

The development of new reverse faults and related folds is strongly controlled by the
mechanical characteristics of the host rocks. In this study we analyze the impact of a specific …

Initiation of subduction is rarely encountered in modern tectonic environments due to its
ephemeral and destructive nature. We report the geological and geophysical evidence …

The kinematics of thrust fault is key to understand the deformation and uplift of mountain
ranges. Along the northern front of the central Qilian Shan mountain range, the NE Tibet …

The thrust sheets of the Northern Calcareous Alps were emplaced during Late Cretaceous
thrust‐dominated transpression expressed by thrust sheets segmented by closely spaced …

Lobate scarps are the topographic expression of the largest thrust faults observed on the
surfaces of terrestrial planets and their study provides information on the mechanical …

We make use of own geological mapping, interpretations of seismic reflection profiles and
deep geophysical data to build a lithospheric-scale cross-section across the European …

Fault-propagation folds are common structures within fold and thrust belts. The trishear
kinematic model has been widely used to understand the kinematics and geometry of these …