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The Neoarchean Uyea Gneiss Complex, Shetland: an onshore fragment of the Rae Craton on the European Plate

View ORCID ProfileP. D. Kinny, R. A. Strachan, View ORCID ProfileM. Fowler, View ORCID ProfileC. Clark, S. Davis, I. Jahn, View ORCID ProfileR. J. M. Taylor, R. E. Holdsworth and E. Dempsey
Journal of the Geological Society, 176, 847-862, 21 June 2019, https://doi.org/10.1144/jgs2019-017
P. D. Kinny
1The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, Perth, WA 6845, Australia
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R. A. Strachan
2School of Earth & Environmental Sciences, University of Portsmouth, Portsmouth PO1 3QL, UK
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M. Fowler
2School of Earth & Environmental Sciences, University of Portsmouth, Portsmouth PO1 3QL, UK
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C. Clark
1The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, Perth, WA 6845, Australia
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S. Davis
1The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, Perth, WA 6845, Australia
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I. Jahn
1The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, Perth, WA 6845, Australia
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R. J. M. Taylor
1The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, Perth, WA 6845, Australia
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R. E. Holdsworth
3Department of Earth Sciences, Durham University, Durham DH1 3LE, UK
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E. Dempsey
4School of Environmental Sciences, University of Hull, Hull HU6 7RX, UK
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Abstract

A tract of amphibolite-facies granitic gneisses and metagabbros in northern Shetland, UK, is here named the Uyea Gneiss Complex. Zircon U–Pb dating indicates emplacement of the igneous protoliths of the complex c. 2746–2726 Ma, at a later time than most of the Archean protoliths of the Lewisian Gneiss Complex of mainland Scotland. Calc-alkaline geochemistry of the Uyea Gneiss Complex indicates arc-affinity and a strong genetic kinship among the mafic and felsic components. Zircon Hf compositions suggest an enriched mantle source and limited interaction with older crust during emplacement. Ductile fabrics developed soon after emplacement, with zircon rims at c. 2710 Ma, but there was little further deformation until Caledonian reworking east of the Uyea Shear Zone. There is no evidence for the Paleoproterozoic reworking that dominates large tracts of the Lewisian Gneiss Complex and of the Nagssugtoqidian Orogen of East Greenland. The more northerly location of the Uyea Gneiss Complex and extensive offshore basement of similar age implies that, prior to the opening of the North Atlantic Ocean, these rocks were contiguous with the Archean Rae Craton.

  • © 2019 The Author(s). Published by The Geological Society of London. All rights reserved
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Journal of the Geological Society: 176 (5)
Journal of the Geological Society
Volume 176, Issue 5
September 2019
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The Neoarchean Uyea Gneiss Complex, Shetland: an onshore fragment of the Rae Craton on the European Plate

P. D. Kinny, R. A. Strachan, M. Fowler, C. Clark, S. Davis, I. Jahn, R. J. M. Taylor, R. E. Holdsworth and E. Dempsey
Journal of the Geological Society, 176, 847-862, 21 June 2019, https://doi.org/10.1144/jgs2019-017
P. D. Kinny
1The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, Perth, WA 6845, Australia
  • Find this author on Google Scholar
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  • ORCID record for P. D. Kinny
  • For correspondence: p.kinny@curtin.edu.au
R. A. Strachan
2School of Earth & Environmental Sciences, University of Portsmouth, Portsmouth PO1 3QL, UK
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M. Fowler
2School of Earth & Environmental Sciences, University of Portsmouth, Portsmouth PO1 3QL, UK
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  • ORCID record for M. Fowler
C. Clark
1The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, Perth, WA 6845, Australia
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  • ORCID record for C. Clark
S. Davis
1The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, Perth, WA 6845, Australia
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I. Jahn
1The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, Perth, WA 6845, Australia
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R. J. M. Taylor
1The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, Perth, WA 6845, Australia
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R. E. Holdsworth
3Department of Earth Sciences, Durham University, Durham DH1 3LE, UK
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E. Dempsey
4School of Environmental Sciences, University of Hull, Hull HU6 7RX, UK
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The Neoarchean Uyea Gneiss Complex, Shetland: an onshore fragment of the Rae Craton on the European Plate

P. D. Kinny, R. A. Strachan, M. Fowler, C. Clark, S. Davis, I. Jahn, R. J. M. Taylor, R. E. Holdsworth and E. Dempsey
Journal of the Geological Society, 176, 847-862, 21 June 2019, https://doi.org/10.1144/jgs2019-017
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