It is suggested that the Mafic Units and HS are allochthonous and were emplaced onto the WGR during an early stage of the Caledonian Orogeny. All units, including the Basement Gneisses, have suffered retrogression during a late extensional phase which continued into at least the Middle Devonian.
| Identifer | oai:union.ndltd.org:bl.uk/oai:ethos.bl.uk:280963 |
| Date | January 1989 |
| Creators | Bailey, David Elliott |
| Contributors | Harley, S. L. |
| Publisher | University of Oxford |
| Source Sets | Ethos UK |
| Detected Language | English |
| Type | Electronic Thesis or Dissertation |
| Source | http://ora.ox.ac.uk/objects/uuid:9c297189-fe46-4d4d-8821-4fce08d5f5cd |
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