In this study, we integrate bedrock datasets, observations of subducted slabs in the mantle,
and plate kinematic constraints to constrain models for the India-Asia collision and the …

The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …

Abstract Closure of the Neotethys Ocean and high-angle continent-continent collision
between India and Asia after about 55 Ma resulted in low-angle subduction of the Indian …

The property of regional metamorphism at convergent plate margins is substantially related
to the change of geothermal gradients, resulting in different types of crustal reworking …

Despite the Mediterranean sector of the Variscan Belt being fragmented and reworked
during Alpine orogenesis, evidence for the activity of a right‐lateral strike‐slip shear zone …

Although the Himalayan orogenic belt is dominant by Oligocene to Miocene leucogranites, it
initiated magmatic activity from middle Eocene. However, the exact distribution and genesis …

This review presents an objective account of metamorphic, microstructural and
geochronological studies in the Greater Himalayan Sequence (GHS) and adjacent units in …

The Himalayan orogen, resulting from the Early Cenozoic collision of the Indian and Asian
plates, is an ideal vehicle to study active orogenic processes and test geodynamic models of …

Abstract Although the India‐Asia collision has been ongoing since the Eocene, the exposed
hinterland of the Himalayan orogen was pervasively deformed and metamorphosed at high …

Abstract The Maures–Tanneron Massif and the Corsica–Sardinia Block are two segments of
the southern European Variscan belt that separated during the Late Oligocene–Miocene …