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SE | Volume 10, issue 3
Solid Earth, 10, 839–850, 2019
https://doi.org/10.5194/se-10-839-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: Understanding the unknowns: the impact of uncertainty in the...

Solid Earth, 10, 839–850, 2019
https://doi.org/10.5194/se-10-839-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 13 Jun 2019

Research article | 13 Jun 2019

Constraining the geotherm beneath the British Isles from Bayesian inversion of Curie depth: integrated modelling of magnetic, geothermal, and seismic data

Ben Mather and Javier Fullea
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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR by Ben Mather on behalf of the Authors (08 May 2019)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (08 May 2019) by Juan Alcalde
AR by Ben Mather on behalf of the Authors (09 May 2019)  Author's response    Manuscript
ED: Publish as is (09 May 2019) by Juan Alcalde
ED: Publish as is (14 May 2019) by CharLotte Krawczyk(Executive Editor)
Publications Copernicus
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Short summary
The temperature in the crust can be constrained by the Curie depth, which is often interpreted as the 580 °C isotherm. We cast the estimation of Curie depth, from maps of the magnetic anomaly, within a Bayesian framework to properly quantify its uncertainty across the British Isles. We find that uncertainty increases considerably for deeper Curie depths, which demonstrates that generally this method is only reliable in hotter regions, such as Scotland and Northern Ireland.
The temperature in the crust can be constrained by the Curie depth, which is often interpreted...
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