Shear zones geometry in the Paraíba do Sul belt, southeastern Brazil, delineates a NE-trending fan-like structure. Shear zones dip towards SE in the northern limb, and towards NW in the southern one. This geometry has been interpreted either due to transpression or to late folding of flat-lying thrust surfaces. Stretching lineation plunges to ENE-ESE in the northern limb and towards NNE-NE in t...

This research assessed stress regimes and fields in eastern Iran using fault-slip data the tectonic events associated with these changes. Our analysis of brittle structures Shekarab Mountains revealed significant changes from late Cretaceous to Quaternary. Reconstructing age sense fault movements showed that during Cretaceous, direction maximum horizontal axes (?1) under a compressional regime ...

The transition along the strike of Sunda subduction zone, from oceanic in west to continental Australian lithosphere east is envisioned as one canonical examples structural changes that take place within an overriding plate when a wedge enters zone. Yet, along-strike offset trench toward margin represents response opposite predictions numerical models. To understand this paradox, we analyse mor...