210 Pb- 226 Ra disequilibria in young gas-laden magmas
We present new 238 U- 230 Th- 226 Ra- 210 Pb and supporting data for young lavas from southwest Pacific island arcs, Eyjafjallajökull, Iceland, and Terceira, Azores. The arc lavas have significant 238 U and 226 Ra excesses, whereas those from the ocean islands have moderate 230 Th and 226 Ra excesse...
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2017
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Online Access: | https://researchers.mq.edu.au/en/publications/ffd9b3b1-82ad-4a71-a4ed-e7ca140905c3 https://doi.org/10.1038/srep45186 https://research-management.mq.edu.au/ws/files/54689131/Publisher_version.pdf http://www.scopus.com/inward/record.url?scp=85016146381&partnerID=8YFLogxK http://purl.org/au-research/grants/arc/DP0988658 http://purl.org/au-research/grants/arc/FT120100440 |
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ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/ffd9b3b1-82ad-4a71-a4ed-e7ca140905c3 2024-10-13T14:07:03+00:00 210 Pb- 226 Ra disequilibria in young gas-laden magmas Reagan, Mark Turner, Simon Handley, Heather Turner, Michael Beier, Christoph Caulfield, John Peate, David 2017-03-24 application/pdf https://researchers.mq.edu.au/en/publications/ffd9b3b1-82ad-4a71-a4ed-e7ca140905c3 https://doi.org/10.1038/srep45186 https://research-management.mq.edu.au/ws/files/54689131/Publisher_version.pdf http://www.scopus.com/inward/record.url?scp=85016146381&partnerID=8YFLogxK http://purl.org/au-research/grants/arc/DP0988658 http://purl.org/au-research/grants/arc/FT120100440 eng eng info:eu-repo/semantics/openAccess Reagan , M , Turner , S , Handley , H , Turner , M , Beier , C , Caulfield , J & Peate , D 2017 , ' 210 Pb- 226 Ra disequilibria in young gas-laden magmas ' , Scientific Reports , vol. 7 , 45186 , pp. 1-12 . https://doi.org/10.1038/srep45186 article 2017 ftmacquarieunicr https://doi.org/10.1038/srep45186 2024-09-18T23:49:09Z We present new 238 U- 230 Th- 226 Ra- 210 Pb and supporting data for young lavas from southwest Pacific island arcs, Eyjafjallajökull, Iceland, and Terceira, Azores. The arc lavas have significant 238 U and 226 Ra excesses, whereas those from the ocean islands have moderate 230 Th and 226 Ra excesses, reflecting mantle melting in the presence of a water-rich fluid in the former and mantle melting by decompression in the latter. Differentiation to erupted compositions in both settings appears to have taken no longer than a few millennia. Variations in the ( 210 Pb/ 226 Ra) 0 values in all settings largely result from degassing processes rather than mineral-melt partitioning. Like most other ocean island basalts, the Terceira basalt has a 210 Pb deficit, which we attribute to ∼8.5 years of steady 222 Rn loss to a CO 2 -rich volatile phase while it traversed the crust. Lavas erupted from water-laden magma systems, including those investigated here, commonly have near equilibrium ( 210 Pb/ 226 Ra) 0 values. Maintaining these equilibrium values requires minimal persistent loss or accumulation of 222 Rn in a gas phase. We infer that degassing during decompression of water-saturated magmas either causes these magmas to crystallize and stall in reservoirs where they reside under conditions of near stasis, or to quickly rise towards the surface and erupt. Article in Journal/Newspaper Eyjafjallajökull Iceland Ocean Island Macquarie University Research Portal Pacific Scientific Reports 7 1 |
institution |
Open Polar |
collection |
Macquarie University Research Portal |
op_collection_id |
ftmacquarieunicr |
language |
English |
description |
We present new 238 U- 230 Th- 226 Ra- 210 Pb and supporting data for young lavas from southwest Pacific island arcs, Eyjafjallajökull, Iceland, and Terceira, Azores. The arc lavas have significant 238 U and 226 Ra excesses, whereas those from the ocean islands have moderate 230 Th and 226 Ra excesses, reflecting mantle melting in the presence of a water-rich fluid in the former and mantle melting by decompression in the latter. Differentiation to erupted compositions in both settings appears to have taken no longer than a few millennia. Variations in the ( 210 Pb/ 226 Ra) 0 values in all settings largely result from degassing processes rather than mineral-melt partitioning. Like most other ocean island basalts, the Terceira basalt has a 210 Pb deficit, which we attribute to ∼8.5 years of steady 222 Rn loss to a CO 2 -rich volatile phase while it traversed the crust. Lavas erupted from water-laden magma systems, including those investigated here, commonly have near equilibrium ( 210 Pb/ 226 Ra) 0 values. Maintaining these equilibrium values requires minimal persistent loss or accumulation of 222 Rn in a gas phase. We infer that degassing during decompression of water-saturated magmas either causes these magmas to crystallize and stall in reservoirs where they reside under conditions of near stasis, or to quickly rise towards the surface and erupt. |
format |
Article in Journal/Newspaper |
author |
Reagan, Mark Turner, Simon Handley, Heather Turner, Michael Beier, Christoph Caulfield, John Peate, David |
spellingShingle |
Reagan, Mark Turner, Simon Handley, Heather Turner, Michael Beier, Christoph Caulfield, John Peate, David 210 Pb- 226 Ra disequilibria in young gas-laden magmas |
author_facet |
Reagan, Mark Turner, Simon Handley, Heather Turner, Michael Beier, Christoph Caulfield, John Peate, David |
author_sort |
Reagan, Mark |
title |
210 Pb- 226 Ra disequilibria in young gas-laden magmas |
title_short |
210 Pb- 226 Ra disequilibria in young gas-laden magmas |
title_full |
210 Pb- 226 Ra disequilibria in young gas-laden magmas |
title_fullStr |
210 Pb- 226 Ra disequilibria in young gas-laden magmas |
title_full_unstemmed |
210 Pb- 226 Ra disequilibria in young gas-laden magmas |
title_sort |
210 pb- 226 ra disequilibria in young gas-laden magmas |
publishDate |
2017 |
url |
https://researchers.mq.edu.au/en/publications/ffd9b3b1-82ad-4a71-a4ed-e7ca140905c3 https://doi.org/10.1038/srep45186 https://research-management.mq.edu.au/ws/files/54689131/Publisher_version.pdf http://www.scopus.com/inward/record.url?scp=85016146381&partnerID=8YFLogxK http://purl.org/au-research/grants/arc/DP0988658 http://purl.org/au-research/grants/arc/FT120100440 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Eyjafjallajökull Iceland Ocean Island |
genre_facet |
Eyjafjallajökull Iceland Ocean Island |
op_source |
Reagan , M , Turner , S , Handley , H , Turner , M , Beier , C , Caulfield , J & Peate , D 2017 , ' 210 Pb- 226 Ra disequilibria in young gas-laden magmas ' , Scientific Reports , vol. 7 , 45186 , pp. 1-12 . https://doi.org/10.1038/srep45186 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1038/srep45186 |
container_title |
Scientific Reports |
container_volume |
7 |
container_issue |
1 |
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1812813311792644096 |