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

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posted on 30.09.2019, 08:44 by M.L. Blades, B.L Alessio, A.S. Collins, J. Foden, J.L. Payne, S. Glorie, P. Holden, B. Thorpe, S. Al-Khirbash
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.

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