This paper reviews the tectonic, magmatic, and metallogenic history of the Tethyan orogen
from the Carpathians to Indochina. Focus is placed on the formation of porphyry Cu±Mo±Au …

Zircon rare earth element (REE) oxy-barometers have been widely used to calculate magma
oxygen fugacity. However, sometimes confusing results are obtained, such as extremely …

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 …

New geochronologic, geochemical, and isotopic data for Mesozoic to Cenozoic igneous
rocks and detrital minerals from the Pamir Mountains help to distinguish major regional …

Observations highlight the complex tectonic, magmatic, and geodynamic phases of the
Cenozoic post-collisional evolution of the Himalayan-Tibetan orogen and show that these …

The E-trending Gangdese porphyry copper belt in southern Tibet is a classic example of
porphyry mineralization in a continental collision zone. New zircon U-Pb geochronological …

This study used clinopyroxene (cpx) compositions and zircon Hf-O isotopes of Eocene
adakitic rocks (EARs) from the Qiangtang block to resolve the mechanism (s) responsible for …

K‐rich adakite‐like rocks (KARs) in post‐collisional settings, such as in Tibet, have been
widely linked with the melting of pre‐existing thickened crust. Here, we investigate …

This study presents new major and trace element, plus Sr–Nd and zircon U–Pb isotope data
for the Zhongcang granitic plutons, which are located to the south of the Yongzhu–Asuo …

Orthopyroxene-bearing granitic rock (eg charnockite) is relatively rare but provides an
excellent opportunity to probe the thermal and tectonic evolution of deep orogenic crust …