Chloride waters of Great Britain revisited: from subsea formation waters to onshore geothermal fluids
It has long been known that chloride-dominated saline ground waters occur at depth in the UK, not only beneath the sea but also onshore at depths of a few hundred metres. In a few places in northern England, these saline waters discharge naturally at surface in the form of springs. In recent years,...
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ftuglasgow:oai:eprints.gla.ac.uk:106365 2023-05-15T17:57:58+02:00 Chloride waters of Great Britain revisited: from subsea formation waters to onshore geothermal fluids Younger, Paul L. Boyce, Adrian J. Waring, Andrew J. 2015-10 text http://eprints.gla.ac.uk/106365/ http://eprints.gla.ac.uk/106365/7/106365.pdf en eng Elsevier Ltd http://eprints.gla.ac.uk/106365/7/106365.pdf Younger, P. L. <http://eprints.gla.ac.uk/view/author/29019.html> , Boyce, A. J. <http://eprints.gla.ac.uk/view/author/1919.html> and Waring, A. J. (2015) Chloride waters of Great Britain revisited: from subsea formation waters to onshore geothermal fluids. Proceedings of the Geologists’ Association <http://eprints.gla.ac.uk/view/journal_volume/Proceedings_of_the_Geologists==2019_Association.html>, 126(4-5), pp. 453-465. (doi:10.1016/j.pgeola.2015.04.001 <http://dx.doi.org/10.1016/j.pgeola.2015.04.001>) cc_by_4 CC-BY Articles PeerReviewed 2015 ftuglasgow https://doi.org/10.1016/j.pgeola.2015.04.001 2020-01-10T00:54:29Z It has long been known that chloride-dominated saline ground waters occur at depth in the UK, not only beneath the sea but also onshore at depths of a few hundred metres. In a few places in northern England, these saline waters discharge naturally at surface in the form of springs. In recent years, however, these saline ground waters have come to be regarded as resources: as potential geothermal fluids intercepted in deep boreholes. Comparisons of the major ions and stable isotopes (δ2H, δ18O and δ34S) of these saline ground waters with North Sea oilfield formation waters, and with brines encountered in former subsea workings of coastal collieries, reveal that they are quite distinct from those found in North Sea oilfields, in that their as δ2H/δ18O signatures are distinctly “meteoric”. δ34S data preclude a significant input from evaporite dissolution – another contrast with many North Sea brines and some colliery waters. Yet, enigmatically, their total dissolved solids contents are far higher than typical meteoric waters. It is tentatively suggested that these paradoxical hydrogeochemical properties might be explained by recharge during Cenozoic uplift episodes, with high concentrations of solutes being derived by a combination of high-temperature rock–water interaction in the radiothermal granites and/or ‘freeze out’ from overlying permafrost that surely formed in this region during cold periods. Geothermometric calculations suggest these saline waters may well be representative of potentially valuable geothermal reservoirs. Article in Journal/Newspaper permafrost University of Glasgow: Enlighten - Publications Proceedings of the Geologists' Association 126 4-5 453 465 |
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Open Polar |
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University of Glasgow: Enlighten - Publications |
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ftuglasgow |
language |
English |
description |
It has long been known that chloride-dominated saline ground waters occur at depth in the UK, not only beneath the sea but also onshore at depths of a few hundred metres. In a few places in northern England, these saline waters discharge naturally at surface in the form of springs. In recent years, however, these saline ground waters have come to be regarded as resources: as potential geothermal fluids intercepted in deep boreholes. Comparisons of the major ions and stable isotopes (δ2H, δ18O and δ34S) of these saline ground waters with North Sea oilfield formation waters, and with brines encountered in former subsea workings of coastal collieries, reveal that they are quite distinct from those found in North Sea oilfields, in that their as δ2H/δ18O signatures are distinctly “meteoric”. δ34S data preclude a significant input from evaporite dissolution – another contrast with many North Sea brines and some colliery waters. Yet, enigmatically, their total dissolved solids contents are far higher than typical meteoric waters. It is tentatively suggested that these paradoxical hydrogeochemical properties might be explained by recharge during Cenozoic uplift episodes, with high concentrations of solutes being derived by a combination of high-temperature rock–water interaction in the radiothermal granites and/or ‘freeze out’ from overlying permafrost that surely formed in this region during cold periods. Geothermometric calculations suggest these saline waters may well be representative of potentially valuable geothermal reservoirs. |
format |
Article in Journal/Newspaper |
author |
Younger, Paul L. Boyce, Adrian J. Waring, Andrew J. |
spellingShingle |
Younger, Paul L. Boyce, Adrian J. Waring, Andrew J. Chloride waters of Great Britain revisited: from subsea formation waters to onshore geothermal fluids |
author_facet |
Younger, Paul L. Boyce, Adrian J. Waring, Andrew J. |
author_sort |
Younger, Paul L. |
title |
Chloride waters of Great Britain revisited: from subsea formation waters to onshore geothermal fluids |
title_short |
Chloride waters of Great Britain revisited: from subsea formation waters to onshore geothermal fluids |
title_full |
Chloride waters of Great Britain revisited: from subsea formation waters to onshore geothermal fluids |
title_fullStr |
Chloride waters of Great Britain revisited: from subsea formation waters to onshore geothermal fluids |
title_full_unstemmed |
Chloride waters of Great Britain revisited: from subsea formation waters to onshore geothermal fluids |
title_sort |
chloride waters of great britain revisited: from subsea formation waters to onshore geothermal fluids |
publisher |
Elsevier Ltd |
publishDate |
2015 |
url |
http://eprints.gla.ac.uk/106365/ http://eprints.gla.ac.uk/106365/7/106365.pdf |
genre |
permafrost |
genre_facet |
permafrost |
op_relation |
http://eprints.gla.ac.uk/106365/7/106365.pdf Younger, P. L. <http://eprints.gla.ac.uk/view/author/29019.html> , Boyce, A. J. <http://eprints.gla.ac.uk/view/author/1919.html> and Waring, A. J. (2015) Chloride waters of Great Britain revisited: from subsea formation waters to onshore geothermal fluids. Proceedings of the Geologists’ Association <http://eprints.gla.ac.uk/view/journal_volume/Proceedings_of_the_Geologists==2019_Association.html>, 126(4-5), pp. 453-465. (doi:10.1016/j.pgeola.2015.04.001 <http://dx.doi.org/10.1016/j.pgeola.2015.04.001>) |
op_rights |
cc_by_4 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1016/j.pgeola.2015.04.001 |
container_title |
Proceedings of the Geologists' Association |
container_volume |
126 |
container_issue |
4-5 |
container_start_page |
453 |
op_container_end_page |
465 |
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1766166493729390592 |