Zircon U-Pb age, whole-rock geochemistry, and in situ isotopic compositions of accessory minerals, for granite and related dioritic rocks from early Cretaceous Shihuzhen-Jiudaogou pluton, Liaodong pe
The Triassic Lincang granites make up the largest peraluminous granitic batholith in the Changning-Menglian Paleo-Tethys orogenic belt, southeastern Tibetan Plateau. It is undoubtedly very important t
Granitic melt composition is controlled by melting reactions and modified by melt segregation process. This is a fundamental but unresolved issue for granite petrogenesis. To investigate the influence
The role of mafic–felsic magma mixing in the formation of granites is controversial. Field evidence in many granite plutons undoubtedly implies interaction of mafic (basaltic–intermediate) magma with
Supplementary table 1: The results of LA-ICP-MS zircon U-Pb dating Supplementary table 2: The results of geochemistry Supplementary table 3: The results of zircon Hf isotope
