Supp Fig 1. Unravelling the Neoproterozoic Accretionary History of Oman, Using an Array of Isotopic Systems in Zircon.
journal contributionposted on 07.11.2019 by M.L. Blades, B.L Alessio, A.S. Collins, J. Foden, J.L. Payne, S. Glorie, P. Holden, B. Thorpe, S. Al-Khirbash
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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.