Probabilistic Surface Heat Flow Estimates Assimilating Paleoclimate History: New Implications for the Thermochemical Structure of Ireland
Regions where surface temperature has increased since past glaciation events, such as Ireland, underestimate the heat output of the Earth unless paleoclimate corrections are applied. We apply probabilistic techniques to quantify the uncertainty of 22 paleoclimate-corrected heat flow estimates in Ire...
Published in: | Journal of Geophysical Research: Solid Earth |
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American Geophysical Union
2018
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Online Access: | https://hdl.handle.net/20.500.14352/94610 https://doi.org/10.1029/2018jb016555 |
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ftunivcmadrid:oai:docta.ucm.es:20.500.14352/94610 2024-09-15T18:20:17+00:00 Probabilistic Surface Heat Flow Estimates Assimilating Paleoclimate History: New Implications for the Thermochemical Structure of Ireland Mather, Ben Farrell, Thomas Fullea Urchulutegui, Javier 2018-11-08 application/pdf https://hdl.handle.net/20.500.14352/94610 https://doi.org/10.1029/2018jb016555 eng eng American Geophysical Union RfPS/2016/50 info:eu-repo/grantAgreement/EC/H2020/657357/EU 16/ERCD/4303 Mather, B. R., Farrell, T. F., & Fullea, J. (2018). Probabilistic surface heat flow estimates assimilating paleoclimate history: New implications for the thermochemical structure of Ireland. Journal of Geophysical Research: Solid Earth, 123, 10,951–10,967. https://doi.org/10.1029/2018JB016555 https://hdl.handle.net/20.500.14352/94610 2169-9313 doi:10.1029/2018jb016555 2169-9356 open access 550.3 Heat flow Paleoclimate Crustal differentiation Ireland British Isles Geofísica 2507 Geofísica journal article VoR 2018 ftunivcmadrid https://doi.org/20.500.14352/9461010.1029/2018jb016555 2024-08-02T03:34:57Z Regions where surface temperature has increased since past glaciation events, such as Ireland, underestimate the heat output of the Earth unless paleoclimate corrections are applied. We apply probabilistic techniques to quantify the uncertainty of 22 paleoclimate-corrected heat flow estimates in Ireland, which assimilate multiple surface temperature histories associated with 130ka of glacial oscillation in the British Isles. Heat flow values increase by approximate to 15mW/m(2) after a paleoclimate correction and provide new insights into the thermochemical structure of the lithosphere. The heat flow regime is broadly delineated by the Iapetus Suture Zone that separates Laurentian to the north and Avalonian terranes to the south (mean surface heat flow of 7314 and 6514mW/m(2), respectively). The degree to which heat-producing elements are partitioned into the uppermost crust is described by the differentiation index of a heat flow province. From Bayesian inversion, we determine that radiogenic elements are substantially more differentiated in the uppermost crust of Laurentia (D-I=2.81.4) than Avalonia (D-I=1.51.3), despite a moderately enriched lower crust (0.8 +/- 0.3W/m(3)). This is facilitated by a thin yet highly radiogenic layer in the uppermost crust of Laurentia (3.9 +/- 1.8W/m(3)). Extrapolating these results across the British Isles and Newfoundland suggests that heat-producing elements have been more successfully reworked into the upper crust to the north of the Iapetus Suture Zone during continental accretion between Laurentia and Avalonia. Irish Research Council for Science, Engineering and Technology Sustainable Energy Authority Of Ireland Marie Sklodowska-Curie Individual Fellowship - Comisión Europea Science Foundation Ireland Depto. de Física de la Tierra y Astrofísica Fac. de Ciencias Físicas TRUE pub Article in Journal/Newspaper Newfoundland Docta Complutense (Universidad Complutense de Madrid - UCM) Journal of Geophysical Research: Solid Earth 123 12 |
institution |
Open Polar |
collection |
Docta Complutense (Universidad Complutense de Madrid - UCM) |
op_collection_id |
ftunivcmadrid |
language |
English |
topic |
550.3 Heat flow Paleoclimate Crustal differentiation Ireland British Isles Geofísica 2507 Geofísica |
spellingShingle |
550.3 Heat flow Paleoclimate Crustal differentiation Ireland British Isles Geofísica 2507 Geofísica Mather, Ben Farrell, Thomas Fullea Urchulutegui, Javier Probabilistic Surface Heat Flow Estimates Assimilating Paleoclimate History: New Implications for the Thermochemical Structure of Ireland |
topic_facet |
550.3 Heat flow Paleoclimate Crustal differentiation Ireland British Isles Geofísica 2507 Geofísica |
description |
Regions where surface temperature has increased since past glaciation events, such as Ireland, underestimate the heat output of the Earth unless paleoclimate corrections are applied. We apply probabilistic techniques to quantify the uncertainty of 22 paleoclimate-corrected heat flow estimates in Ireland, which assimilate multiple surface temperature histories associated with 130ka of glacial oscillation in the British Isles. Heat flow values increase by approximate to 15mW/m(2) after a paleoclimate correction and provide new insights into the thermochemical structure of the lithosphere. The heat flow regime is broadly delineated by the Iapetus Suture Zone that separates Laurentian to the north and Avalonian terranes to the south (mean surface heat flow of 7314 and 6514mW/m(2), respectively). The degree to which heat-producing elements are partitioned into the uppermost crust is described by the differentiation index of a heat flow province. From Bayesian inversion, we determine that radiogenic elements are substantially more differentiated in the uppermost crust of Laurentia (D-I=2.81.4) than Avalonia (D-I=1.51.3), despite a moderately enriched lower crust (0.8 +/- 0.3W/m(3)). This is facilitated by a thin yet highly radiogenic layer in the uppermost crust of Laurentia (3.9 +/- 1.8W/m(3)). Extrapolating these results across the British Isles and Newfoundland suggests that heat-producing elements have been more successfully reworked into the upper crust to the north of the Iapetus Suture Zone during continental accretion between Laurentia and Avalonia. Irish Research Council for Science, Engineering and Technology Sustainable Energy Authority Of Ireland Marie Sklodowska-Curie Individual Fellowship - Comisión Europea Science Foundation Ireland Depto. de Física de la Tierra y Astrofísica Fac. de Ciencias Físicas TRUE pub |
format |
Article in Journal/Newspaper |
author |
Mather, Ben Farrell, Thomas Fullea Urchulutegui, Javier |
author_facet |
Mather, Ben Farrell, Thomas Fullea Urchulutegui, Javier |
author_sort |
Mather, Ben |
title |
Probabilistic Surface Heat Flow Estimates Assimilating Paleoclimate History: New Implications for the Thermochemical Structure of Ireland |
title_short |
Probabilistic Surface Heat Flow Estimates Assimilating Paleoclimate History: New Implications for the Thermochemical Structure of Ireland |
title_full |
Probabilistic Surface Heat Flow Estimates Assimilating Paleoclimate History: New Implications for the Thermochemical Structure of Ireland |
title_fullStr |
Probabilistic Surface Heat Flow Estimates Assimilating Paleoclimate History: New Implications for the Thermochemical Structure of Ireland |
title_full_unstemmed |
Probabilistic Surface Heat Flow Estimates Assimilating Paleoclimate History: New Implications for the Thermochemical Structure of Ireland |
title_sort |
probabilistic surface heat flow estimates assimilating paleoclimate history: new implications for the thermochemical structure of ireland |
publisher |
American Geophysical Union |
publishDate |
2018 |
url |
https://hdl.handle.net/20.500.14352/94610 https://doi.org/10.1029/2018jb016555 |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_relation |
RfPS/2016/50 info:eu-repo/grantAgreement/EC/H2020/657357/EU 16/ERCD/4303 Mather, B. R., Farrell, T. F., & Fullea, J. (2018). Probabilistic surface heat flow estimates assimilating paleoclimate history: New implications for the thermochemical structure of Ireland. Journal of Geophysical Research: Solid Earth, 123, 10,951–10,967. https://doi.org/10.1029/2018JB016555 https://hdl.handle.net/20.500.14352/94610 2169-9313 doi:10.1029/2018jb016555 2169-9356 |
op_rights |
open access |
op_doi |
https://doi.org/20.500.14352/9461010.1029/2018jb016555 |
container_title |
Journal of Geophysical Research: Solid Earth |
container_volume |
123 |
container_issue |
12 |
_version_ |
1810458657453768704 |