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 …

Eclogites and granulites are fossil records of orogenies and provide crucial evidence of
geodynamic processes. Incomplete knowledge on both hampers the establishment of …

Revealing the timescales of metamorphic and anatectic processes is central to our
understanding of tectonic evolution of collisional orogens. High‐temperature migmatites and …

The timing of high-pressure (HP) metamorphism in the eastern Himalayan syntaxis is
important for understanding the India-Asia collisional processes, but it remains elusive. To …

The bulk composition of overthickened Tibetan deep crust has been generally believed to
be mafic granulite with eclogite at the lowermost crust. However, a granulitic/eclogitic deep …