Gondwana break-up related magmatism in the Falkland Islands
Jurassic dykes (c. 182 Ma) are widespread across the Falkland Islands and exhibit considerable geochemical variability. Orthopyroxene-bearing NW–SE-oriented quartz-tholeiite dykes underwent fractional crystallization at >1 GPa, and major element constraints suggest that they were derived by melti...
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ftopenunivgb:oai:oro.open.ac.uk:44332 2023-06-11T04:07:05+02:00 Gondwana break-up related magmatism in the Falkland Islands Hole, M. J. Ellam, R. M. MacDonald, D. I. M. Kelley, S. P. 2015 application/pdf https://oro.open.ac.uk/44332/ https://oro.open.ac.uk/44332/1/Hole%20Ellam%20MacDonald%20and%20Kelley.pdf https://doi.org/10.1144/jgs2015-027 unknown https://oro.open.ac.uk/44332/1/Hole%20Ellam%20MacDonald%20and%20Kelley.pdf Hole, M. J.; Ellam, R. M.; MacDonald, D. I. M. and Kelley, S. P. <http://oro.open.ac.uk/view/person/spk5.html> (2015). Gondwana break-up related magmatism in the Falkland Islands. Journal of the Geological Society, 173(1) pp. 108–126. Journal Item Public PeerReviewed 2015 ftopenunivgb https://doi.org/10.1144/jgs2015-027 2023-05-28T05:53:11Z Jurassic dykes (c. 182 Ma) are widespread across the Falkland Islands and exhibit considerable geochemical variability. Orthopyroxene-bearing NW–SE-oriented quartz-tholeiite dykes underwent fractional crystallization at >1 GPa, and major element constraints suggest that they were derived by melting of a pyroxenite-rich source. They have εNd 182 in the range –6 to –11 and 87 Sr/ 86 Sr 182 >0.710 and therefore require an old lithospheric component in their source. A suite of basaltic andesites and andesites exhibit geochemical compositions transitional between Ferrar and Karoo magma types, and are similar to those seen in the KwaZulu-Natal region of southern Africa and the Theron Mountains of Antarctica. Olivine-phyric intrusions equilibrated at <0.5 GPa, and have isotopic compositions (εNd 182 1.6–3.6 and 87 Sr/ 86 Sr 182 0.7036–0.7058) that require limited interaction with old continental lithosphere. A suite of plagioclase-phyric intrusions with 87 Sr/ 86 Sr 182 c. 0.7035 and εNd 182 c. +4, and low Th/Ta and La/Ta ratios (c. 1 and c. 15, respectively) also largely escaped interaction with the lithosphere. These isotopically depleted intrusions were probably emplaced synchronously with Gondwana fragmentation and the formation of new oceanic lithosphere. Estimates of mantle potential temperature from olivine equilibration temperatures do not provide unequivocal evidence for the presence of a plume thermal anomaly beneath the Falkland Islands at 182 Ma. Article in Journal/Newspaper Antarc* Antarctica The Open University: Open Research Online (ORO) Theron Mountains ENVELOPE(-28.068,-28.068,-79.044,-79.044) Journal of the Geological Society 173 1 108 126 |
institution |
Open Polar |
collection |
The Open University: Open Research Online (ORO) |
op_collection_id |
ftopenunivgb |
language |
unknown |
description |
Jurassic dykes (c. 182 Ma) are widespread across the Falkland Islands and exhibit considerable geochemical variability. Orthopyroxene-bearing NW–SE-oriented quartz-tholeiite dykes underwent fractional crystallization at >1 GPa, and major element constraints suggest that they were derived by melting of a pyroxenite-rich source. They have εNd 182 in the range –6 to –11 and 87 Sr/ 86 Sr 182 >0.710 and therefore require an old lithospheric component in their source. A suite of basaltic andesites and andesites exhibit geochemical compositions transitional between Ferrar and Karoo magma types, and are similar to those seen in the KwaZulu-Natal region of southern Africa and the Theron Mountains of Antarctica. Olivine-phyric intrusions equilibrated at <0.5 GPa, and have isotopic compositions (εNd 182 1.6–3.6 and 87 Sr/ 86 Sr 182 0.7036–0.7058) that require limited interaction with old continental lithosphere. A suite of plagioclase-phyric intrusions with 87 Sr/ 86 Sr 182 c. 0.7035 and εNd 182 c. +4, and low Th/Ta and La/Ta ratios (c. 1 and c. 15, respectively) also largely escaped interaction with the lithosphere. These isotopically depleted intrusions were probably emplaced synchronously with Gondwana fragmentation and the formation of new oceanic lithosphere. Estimates of mantle potential temperature from olivine equilibration temperatures do not provide unequivocal evidence for the presence of a plume thermal anomaly beneath the Falkland Islands at 182 Ma. |
format |
Article in Journal/Newspaper |
author |
Hole, M. J. Ellam, R. M. MacDonald, D. I. M. Kelley, S. P. |
spellingShingle |
Hole, M. J. Ellam, R. M. MacDonald, D. I. M. Kelley, S. P. Gondwana break-up related magmatism in the Falkland Islands |
author_facet |
Hole, M. J. Ellam, R. M. MacDonald, D. I. M. Kelley, S. P. |
author_sort |
Hole, M. J. |
title |
Gondwana break-up related magmatism in the Falkland Islands |
title_short |
Gondwana break-up related magmatism in the Falkland Islands |
title_full |
Gondwana break-up related magmatism in the Falkland Islands |
title_fullStr |
Gondwana break-up related magmatism in the Falkland Islands |
title_full_unstemmed |
Gondwana break-up related magmatism in the Falkland Islands |
title_sort |
gondwana break-up related magmatism in the falkland islands |
publishDate |
2015 |
url |
https://oro.open.ac.uk/44332/ https://oro.open.ac.uk/44332/1/Hole%20Ellam%20MacDonald%20and%20Kelley.pdf https://doi.org/10.1144/jgs2015-027 |
long_lat |
ENVELOPE(-28.068,-28.068,-79.044,-79.044) |
geographic |
Theron Mountains |
geographic_facet |
Theron Mountains |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_relation |
https://oro.open.ac.uk/44332/1/Hole%20Ellam%20MacDonald%20and%20Kelley.pdf Hole, M. J.; Ellam, R. M.; MacDonald, D. I. M. and Kelley, S. P. <http://oro.open.ac.uk/view/person/spk5.html> (2015). Gondwana break-up related magmatism in the Falkland Islands. Journal of the Geological Society, 173(1) pp. 108–126. |
op_doi |
https://doi.org/10.1144/jgs2015-027 |
container_title |
Journal of the Geological Society |
container_volume |
173 |
container_issue |
1 |
container_start_page |
108 |
op_container_end_page |
126 |
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1768379682730803200 |