Supp Fig 1. Unravelling the Neoproterozoic Accretionary History of Oman, Using an Array of Isotopic Systems in Zircon.

Fig. 1: Weighted average plots (>90% concordant) of zircon ages from all igneous basement samples in Oman. Black bars are ²⁰⁶Pb/²³⁸U ages with 2σ errors. Grey bars (corresponding to either ²⁰⁷Pb/²⁰⁶Pb, dark grey or ²⁰⁶Pb/²³⁸U (light grey)) weighted averages ages 2σ errors. Where there are multiple populations interpreted these are shown by a second weighted average age and mean, however only the crystallisation age is quoted in the figure. These plots are used to highlight any trends in the data.