The continental crust in the overriding plate of the India-Asia collision zone in southern Tibet
is characterized by an overthickened layer of felsic composition with an underlying granulite …

The Lhasa terrane is widely regarded as an integral unit that separated from Gondwana in
the Carboniferous or late Triassic, but this terrane may more reasonably consist of two …

Previous models related to ultrapotassic mantle and post-collisional porphyry Cu
mineralization have been challenged by the newly identified ultrapotassic lamprophyres …

Magmatic arcs are natural laboratories for studying the growth of continental crusts. The
Gangdese arc, southern Tibet, is an archetypal continental magmatic arc that formed due to …

Collision-induced subduction transference may have triggered subduction of the Neo-Tethys
oceanic lithosphere. To verify this proposition, we present an integrated geochemical and …

The Mo stable isotope system has been used to trace material recycling during subduction-
related processes, but the behavior of Mo isotopes during magmatic evolution (eg, crystal …

Studies of accreted oceanic plateau sections provide crucial information on their structures,
compositions, and origins. We investigate the petrogenesis of ultramafic–mafic rocks in the …

The temporal and spatial distribution of enriched source components at sites of continent–
continent collision provides critical insights into mantle dynamic processes associated with …

Abstract The Tibetan Plateau is one of the most significant Cu poly-metallic mineralization
regions in the world and preserves important information related to subductional and …

In the Gangdese magmatic belt of southern Tibet, widespread Late Mesozoic magmatism
has been reported, although their petrogenesis and tectonic evolution remain ambiguous …