Mid-Eocene renewal of magmatism in NW Scotland: the Loch Roag Dyke, Outer Hebrides
A monchquite dyke, in the vicinity of Loch Roag, Lewis, Outer Hebrides has an unusually enriched chemistry, and contains a unique assemblage of megacrysts and xenoliths from the lithosphere of the Hebridean craton. A 40Ar/39Ar plateau age of 45.2 ± 0.2 Ma (2σ) of a phlogopite megacryst from the dyke...
Published in: | Journal of the Geological Society |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2012
|
Subjects: | |
Online Access: | http://eprints.gla.ac.uk/60700/ https://doi.org/10.1144/0016-76492011-117 |
id |
ftuglasgow:oai:eprints.gla.ac.uk:60700 |
---|---|
record_format |
openpolar |
spelling |
ftuglasgow:oai:eprints.gla.ac.uk:60700 2023-05-15T16:03:40+02:00 Mid-Eocene renewal of magmatism in NW Scotland: the Loch Roag Dyke, Outer Hebrides Faithfull, J.W. Timmerman, M.J. Upton, B.G.J. Rumsey, M.S. 2012 http://eprints.gla.ac.uk/60700/ https://doi.org/10.1144/0016-76492011-117 unknown Faithfull, J.W. <http://eprints.gla.ac.uk/view/author/8006.html> , Timmerman, M.J., Upton, B.G.J. and Rumsey, M.S. (2012) Mid-Eocene renewal of magmatism in NW Scotland: the Loch Roag Dyke, Outer Hebrides. Journal of the Geological Society <http://eprints.gla.ac.uk/view/journal_volume/Journal_of_the_Geological_Society.html>, 169(2), pp. 115-118. (doi:10.1144/0016-76492011-117 <http://dx.doi.org/10.1144/0016-76492011-117>) Articles PeerReviewed 2012 ftuglasgow https://doi.org/10.1144/0016-76492011-117 2021-09-23T22:40:00Z A monchquite dyke, in the vicinity of Loch Roag, Lewis, Outer Hebrides has an unusually enriched chemistry, and contains a unique assemblage of megacrysts and xenoliths from the lithosphere of the Hebridean craton. A 40Ar/39Ar plateau age of 45.2 ± 0.2 Ma (2σ) of a phlogopite megacryst from the dyke overlaps an earlier reported K–Ar age, and confirms that the British Palaeogene Igneous Province extended into the Eocene. Similar late low-volume melts were erupted in the Eocene and Oligocene in West and East Greenland, suggesting that such late-stage magmatic rejuvenescence is a widespread feature across the North Atlantic Igneous Province. Article in Journal/Newspaper East Greenland Greenland North Atlantic University of Glasgow: Enlighten - Publications Greenland Journal of the Geological Society 169 2 115 118 |
institution |
Open Polar |
collection |
University of Glasgow: Enlighten - Publications |
op_collection_id |
ftuglasgow |
language |
unknown |
description |
A monchquite dyke, in the vicinity of Loch Roag, Lewis, Outer Hebrides has an unusually enriched chemistry, and contains a unique assemblage of megacrysts and xenoliths from the lithosphere of the Hebridean craton. A 40Ar/39Ar plateau age of 45.2 ± 0.2 Ma (2σ) of a phlogopite megacryst from the dyke overlaps an earlier reported K–Ar age, and confirms that the British Palaeogene Igneous Province extended into the Eocene. Similar late low-volume melts were erupted in the Eocene and Oligocene in West and East Greenland, suggesting that such late-stage magmatic rejuvenescence is a widespread feature across the North Atlantic Igneous Province. |
format |
Article in Journal/Newspaper |
author |
Faithfull, J.W. Timmerman, M.J. Upton, B.G.J. Rumsey, M.S. |
spellingShingle |
Faithfull, J.W. Timmerman, M.J. Upton, B.G.J. Rumsey, M.S. Mid-Eocene renewal of magmatism in NW Scotland: the Loch Roag Dyke, Outer Hebrides |
author_facet |
Faithfull, J.W. Timmerman, M.J. Upton, B.G.J. Rumsey, M.S. |
author_sort |
Faithfull, J.W. |
title |
Mid-Eocene renewal of magmatism in NW Scotland: the Loch Roag Dyke, Outer Hebrides |
title_short |
Mid-Eocene renewal of magmatism in NW Scotland: the Loch Roag Dyke, Outer Hebrides |
title_full |
Mid-Eocene renewal of magmatism in NW Scotland: the Loch Roag Dyke, Outer Hebrides |
title_fullStr |
Mid-Eocene renewal of magmatism in NW Scotland: the Loch Roag Dyke, Outer Hebrides |
title_full_unstemmed |
Mid-Eocene renewal of magmatism in NW Scotland: the Loch Roag Dyke, Outer Hebrides |
title_sort |
mid-eocene renewal of magmatism in nw scotland: the loch roag dyke, outer hebrides |
publishDate |
2012 |
url |
http://eprints.gla.ac.uk/60700/ https://doi.org/10.1144/0016-76492011-117 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
East Greenland Greenland North Atlantic |
genre_facet |
East Greenland Greenland North Atlantic |
op_relation |
Faithfull, J.W. <http://eprints.gla.ac.uk/view/author/8006.html> , Timmerman, M.J., Upton, B.G.J. and Rumsey, M.S. (2012) Mid-Eocene renewal of magmatism in NW Scotland: the Loch Roag Dyke, Outer Hebrides. Journal of the Geological Society <http://eprints.gla.ac.uk/view/journal_volume/Journal_of_the_Geological_Society.html>, 169(2), pp. 115-118. (doi:10.1144/0016-76492011-117 <http://dx.doi.org/10.1144/0016-76492011-117>) |
op_doi |
https://doi.org/10.1144/0016-76492011-117 |
container_title |
Journal of the Geological Society |
container_volume |
169 |
container_issue |
2 |
container_start_page |
115 |
op_container_end_page |
118 |
_version_ |
1766399373980205056 |