The concepts of progressive and polyphase deformation have been widely applied by
structural geologists to explain complexly deformed rocks, particularly for ductile conditions …

Opposite shear sense (OSS) is manifested by the presence of conflicting shear sense
indicators in a portion of a rock body, a shear/fault zone or across several parallel shear/fault …

Several extrusion mechanisms have been proposed to explain the occurrences of ultra-high
pressure (UHP) rocks at collisional margins. Here we assess the suitability of the channel …

Dating the timing of ductile shear deformation is critical to the understanding of complex,
multi‐episode kinematics that commonly occur within the study of continental tectonics. The …

Abstract The Daling Thrust (DT) delineates a zone of intense shear localization in the Lesser
Himalayan Sequence (LHS) of the Darjeeling–Sikkim Himalaya. From microstructural …

Quartz c‐axis fabrics in natural mylonites can vary to such an extent that they apparently
give opposite senses of shear in a single thin section. Many hypotheses have been invoked …

New quartz texture and c-axis fabric data from across the Paleoproterozoic Ulleri-Phaplu-
Melung orthogneiss in the Khimti Khola region of east central Nepal provide new constraints …

The Almyropotamos tectonic window on southern Evia island in the NW Aegean Sea divides
two high pressure‐low temperature metamorphic units, representing distinct Hellenic thrust …

Dating the timing of deformation within shear zones is critical to quantifying orogenic
processes and developing time-resolved regional tectonic frameworks. Such work requires …

This study was performed on the preliminary geoheritage assessment of the Gharam
Chashma Granitic Batholith (GCGB) based on field observations, petrology, and the …