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

Blades, M.L.; Alessio, B.L; Collins, A.S.; Foden, J.; Payne, J.L.; Glorie, S.; Holden, P.; Thorpe, B.; Al-Khirbash, S.

doi:10.6084/m9.figshare.9918617.v1

jgs2018-125_si_006.pdf (420.16 kB)

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

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posted on 2019-09-30, 08:44 authored 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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Pb-loss trends Hf Isotopic Systems Oman Supp Fig Zircon sample 2. Unravelling zircon Neoproterozoic Accretionary History Array Geology

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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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