Fig. A.5. Two parallel magmatic belts with contrasting isotopic characteristics from southern Tibet to Myanmar: Zircon U–Pb and Hf isotopic constraints

Fig. A.5. Plots of εNd (T) values vs. initial Sr isotope ratios for the samples from Myanmar. For comparison, the data of the Tengchong block from Liu et al. (2009), Monywa and Popa volcanos from Yang (2008), and the eastern Transhimalayan batholith, SE Tibet from Lin et al. (2012) are also shown.