This contribution is a synthesis of studies carried out since 2004 in the Makran accretionary
wedge exposed in SE Iran. These studies were intended to improve our understanding of …

Abstract The Indo-Burma Ranges form an enigmatic mountain belt, with fragments of
evidence for an early accretionary history (Jurassic Jade belt HP-LT metamorphism; Early …

The intricate convergence of tectonic plates and the interplay between landmasses and
oceans in subduction zones give rise to marine geo-hazards, encompassing catastrophic …

The Makran subduction zone is segmented into western and eastern parts. The small
number of teleseismic and regionally-recorded earthquakes makes it difficult to detect …

Contractional relay zones between pairs of normal faults are sometimes associated with
multiple antithetic faults in a geometry similar to that found in Riedel shear zones. Detailed …

Examples of atypical syn-collisional wedges from offshore Sabah and Palawan, Indo-Burma
Ranges, Gibraltar Arc, Banda Arc resemble accretionary prisms, but formed over subducted …

The complex interplay between thrust wedge deformation, tectonically-induced fluid
overpressures, and the complex phases of wedge-top sedimentary depositional systems in …

Abstract The Makran Subduction Zone is the primary seismic/tsunami hazard of the
northwestern Indian Ocean, but little is known of its on‐shore seismic structure. We derived a …

Over time, river networks achieve a specific pattern as determined by the function of several
factors such as climate, tectonic, geological structures, topography, lithology, and base-level …

Deepwater fold-thrust belts (FTBs) are predominantly formed by the deformation of
sedimentary sequences as a result of subduction of oceanic plates at active margins …