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 ε<sub>Nd</sub> (T) values vs. initial Sr isotope ratios for the samples from Myanmar. For comparison, the data of the Tengchong block from Liu <i>et al.</i> (2009), Monywa and Popa volcanos from Yang (2008), and the eastern Transhimalayan batholith, SE Tibet from Lin <i>et al.</i> (2012) are also shown.