Palaeoproterozoic terrane assembly in the Lewisian Gneiss Complex on the Scottish mainland, south of Gruinard Bay: SHRIMP U–Pb zircon evidence
New SHRIMP U–Pb zircon geochronology and fieldwork integrated with reappraisal of earlier mapping demonstrates that the so-called ‘southern region’ of the mainland Lewisian Gneiss Complex comprises a package of distinct tectono-stratigraphic units. From south to north these are the Rona (3135–2889 M...
| Main Authors: | , , |
|---|---|
| Format: | Journal Article |
| Published: |
Elsevier Science BV
2010
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/42414 |