The tectonic affinities of terranes in accretionary orogens can be evaluated using geochronological techniques. U-Pb zircon data obtained from paragneisses of the Coedana Complex (Anglesey) and the Malverns Complex, southern Britain, indicate that they were deposited during the mid- to late Neoproterozoic and have a comparable Amazonian provenance. Metamorphism of the Coedana gneisses occurred at 666 ± 7 Ma, similar to the age of metamorphism in the Malverns Complex. Anglesey therefore probably evolved in proximity to the Avalonian basement of mainland southern Britain during the mid- to late Neoproterozoic and is not a 'suspect terrane' relative to the remainder of Avalonia.
CITATION STYLE
Strachan, R. A., Collins, A. S., Buchan, C., Nance, R. D., Murphy, J. B., & D’Lemos, R. S. (2007). Terrane analysis along a Neoproterozoic active margin of Gondwana: Insights from U-Pb zircon geochronology. Journal of the Geological Society, 164(1), 57–60. https://doi.org/10.1144/0016-76492006-014
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