Supp Fig. 2. Unravelling the Neoproterozoic Accretionary History of Oman, Using an Array of Isotopic Systems in Zircon.

Fig. 2 Initial ¹⁷⁶Hf/¹⁷⁷Hf versus ²⁰⁶Pb/²³⁸U age for zircon in all igneous samples. These are used to identify any distinct Pb-loss trends that appear as a horizontal trend on the plot.