Data for: Origin and Evolution of the Neoproterozoic Dengganping Granitic Complex in the western margin of the Yangtze Block, SW China: implications for Breakup of Rodina Supercontinent

This contribution presents new magmatic zircon U–Pb geochronology, Hf-O isotope and whole rock Nd isotope to constraints on the origin and tectonic setting of the Dengganping Complex along the western margin of the Yangtze Block. The results of and geochemistry provide a better understanding of the tectonic setting for the Neoproterozoic magmatic rocks in the study area, which are placed in context with the breakup of the Rodinia Supercontinent.