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Table S1. U–Pb isotopic data. Patterns of Silurian deformation and magmatism during sinistral oblique convergence, northern Scottish Caledonides.

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posted on 2020-05-04, 07:47 authored by R.A. Strachan, G.I. Alsop, J. Ramezani, R.E. Frazer, I.M. Burns, R.E. Holdsworth
Table S1. U–Pb isotopic data.

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    Journal of the Geological Society

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    Keywords

    Silurian deformationScottish CaledonidesPatternsinistralmagmatismconvergencedata1.Geology

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