The Menghai batholith (Yunnan Province, China) is the southern extension of the ~370 km long Lincang granite body that syntectonically intruded the collisional zone between Gondwana (Baoshan block) an
Continental alkaline basalts of Eocene to Pleistocene age erupted in the back-arc of Patagonian Argentina east of a seismic and volcanic gap in the Andes.
The whole-rock geochemistry and zircon Hf-O isotopic data, zircon U-Pb dating, major and trace elements chosen for thermodynamic simulations and trace element characteristics modelling in the study. T