The Himalayan orogen is an archetype of collisional orogens built by the continental
collision between India and Asia in the Cenozoic, and it has been a natural laboratory for …

The battery metals tin and lithium (Snsingle bondLi) are key to renewable energy
technologies, with demand driving new interest in the formation and exploration of tin …

The relationship between fluid activity and anatexis in the Himalaya is ambiguous in regard
to whether it is dominated by fluid-saturated melting triggered by Lesser Himalayan …

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

Re-examination of three specimens from the Kanchenjunga Himal of Nepal via in situ Lu-Hf
garnet geochronology yields evidence of multiple garnet growth events. Spot analyses from …

Crustal anatexis in collisional orogens has great bearing on geochemical differentiation of
the continental crust. However, it is often uncertain what kind of crustal rocks were partially …

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 …

Abstract The Sandmata Complex in the Aravalli Craton of northwestern India experienced
syn-to post-collisional high-grade metamorphism and migmatization related to the 1.9–1.7 …

Determining the sources and the evolution of the Himalayan leucogranites is crucial to
deciphering the teotono-magmatic evolution history of the Himalayan Orogen. Various …

Abstract Sitting between the Greater Himalayan sequence (GHS) and Lesser Himalayan
sequence (LHS), the Main Central Thrust zone (MCTZ) has experienced multiple episodes …