Provenance of the Highland Border Complex: constraints on Laurentian marginaccretion in the Scottish Caledonides
Contrasting tectonic models for the Highland Border Complex in the Scottish Caledonides view it either as part of the rifted Laurentian margin of the Iapetus Ocean or as an oceanic terrane. Detrital zircon data from sandstones of the complex yield age peaks at 2.8–2.6, 1.3 and 1.1–1.0 Ga and minor p...
| Main Authors: | , , , |
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| Format: | Journal Article |
| Published: |
Geological Society of London
2012
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| Online Access: | http://hdl.handle.net/20.500.11937/3999 |