Origin and evolution of the Tengchong block, southeastern margin of the Tibetan Plateau: Zircon U–Pb and Lu–Hf isotopic evidence from the (meta-) sedimentary rocks and intrusions
Origin and evolution of the Tengchong block, southeastern margin of the Tibetan Plateau: Zircon U–Pb and Lu–Hf isotopic evidence from the (meta-) sedimentary rocks and intrusions
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