Institute for Geophysics and Tectonics, School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, United Kingdom
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Total article views: 5,456 (including HTML, PDF, and XML)
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4,043
1,249
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PDF: 1,249
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Total: 5,456
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EndNote: 334
Views and downloads (calculated since 22 Aug 2022)
Cumulative views and downloads
(calculated since 22 Aug 2022)
Total article views: 4,684 (including HTML, PDF, and XML)
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EndNote
3,288
1,234
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4,684
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HTML: 3,288
PDF: 1,234
XML: 162
Total: 4,684
Supplement: 266
BibTeX: 262
EndNote: 319
Views and downloads (calculated since 11 Jul 2023)
Cumulative views and downloads
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Total article views: 772 (including HTML, PDF, and XML)
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755
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BibTeX: 13
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Views and downloads (calculated since 22 Aug 2022)
Cumulative views and downloads
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Viewed (geographical distribution)
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 5,456 (including HTML, PDF, and XML)
Thereof 5,206 with geography defined
and 250 with unknown origin.
Total article views: 4,684 (including HTML, PDF, and XML)
Thereof 4,447 with geography defined
and 237 with unknown origin.
Total article views: 772 (including HTML, PDF, and XML)
Thereof 759 with geography defined
and 13 with unknown origin.
A common simplification in subduction zone models is the use of constant thermal parameters, while experiments have shown that they vary with temperature. We test various formulations of temperature-dependent thermal parameters and show that they change the thermal structure of the subducting slab. We recommend that modelling studies of the thermal structure of subduction zones take the temperature dependence of thermal parameters into account, especially when providing insights into seismicity.
A common simplification in subduction zone models is the use of constant thermal parameters,...
