摘要
The nature of magma source region and petrogenesis of the Nyainrong pluton in northern Tibet remain poorly constrained, consequently raising uncertainties for understanding the tectonomagmatic evolution of the Bangong-Nujiang suture zone during the Early Jurassic. To explore these issues, this paper reports the petrological, whole-rock geochemical, zircon U-Pb dating, and zircon Lu-Hf isotopic data of host granites and dioritic enclaves from the Nyainrong pluton. The results imply in turn that the Bangong-Nujiang Ocean seafloors may have subducted southward towards beneath the Lhasa Terrane and also subducted northward towards beneath the Qiangtang Terrane.