Data for: Compositional changes of granitoids from the Menglian Batholith in SW China at ca. 122 Ma: Implications for the origin of decoupled Nd–Hf isotopic compositions and crust generation in collision zones

Published: 26 April 2021| Version 1 | DOI: 10.17632/trh8mmxf5x.1
Contributor:
Di-Cheng Zhu

Description

Zircon U-Pb age, major and trace elements, and whole-rock geochemical data of the Menglian Batholith, SW Yunnan

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