Fold-and-thrust belts and accretionary wedges form by compression of sedimentary sequences and basement rocks into forward and backward thrusts, folds, nappes, and …
Thin‐skinned fold‐and‐thrust belts related to convergence tectonics develop by scraping off a rock sequence along a weaker basal décollement often formed by water‐saturated shale …
P Santolaria, P Granado, EP Wilson, M de Matteis… - …, 2022 - Wiley Online Library
Analog modeling is used to study the role played by the inherited salt‐sediment architecture of a salt‐bearing rifted margin, developed by minibasin downbuilding and margin‐scale …
A line-length balanced palinspastic reconstruction across the Himachal Himalaya is presented, highlighting different phases of Himalayan tectonic development: Eocene …
The Zagros fold-thrust belt in the Kurdistan region of Iraq encroached southward toward a rapidly subsiding Neogene foreland basin and was later partitioned by out-of-sequence …
Orogenic wedges commonly display an inner wedge, where crystalline units have been exhumed, and an outer wedge formed by imbricated sedimentary units detached from the …
Erosion, sediment production, and routing on a tectonically active continental margin reflect both tectonic and climatic processes; partitioning the relative importance of these processes …
Contractional deformation in the outer parts of fold‐and‐thrust belts is in part controlled by the presence of syntectonic sediments and multiple décollements (eg, the Apennines, the …
JP Burg, A Dolati, D Bernoulli, J Smit - Lithosphere dynamics and …, 2013 - Springer
We report new structural descriptions and measurements carried out across the onshore Makran Accretionary Wedge, in SE Iran. Complementary geological mapping led to the …