Department of Earth Sciences, Utrecht University, Princetonlaan 8A, 3584 CB Utrecht, the Netherlands
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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: 3,217 (including HTML, PDF, and XML)
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2,320
705
192
3,217
186
224
HTML: 2,320
PDF: 705
XML: 192
Total: 3,217
BibTeX: 186
EndNote: 224
Views and downloads (calculated since 12 Dec 2023)
Cumulative views and downloads
(calculated since 12 Dec 2023)
Total article views: 2,222 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,336
705
181
2,222
186
224
HTML: 1,336
PDF: 705
XML: 181
Total: 2,222
BibTeX: 186
EndNote: 224
Views and downloads (calculated since 19 Jul 2024)
Cumulative views and downloads
(calculated since 19 Jul 2024)
Total article views: 995 (including HTML, PDF, and XML)
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984
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11
995
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Total: 995
BibTeX: 0
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Views and downloads (calculated since 12 Dec 2023)
Cumulative views and downloads
(calculated since 12 Dec 2023)
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: 3,217 (including HTML, PDF, and XML)
Thereof 3,128 with geography defined
and 89 with unknown origin.
Total article views: 2,222 (including HTML, PDF, and XML)
Thereof 2,145 with geography defined
and 77 with unknown origin.
Total article views: 995 (including HTML, PDF, and XML)
Thereof 983 with geography defined
and 12 with unknown origin.
Geodynamic models of mantle convection provide a powerful tool to study the structure and composition of the Earth's mantle. Comparing such models with other datasets is difficult. We explore the use of configurational entropy, which allows us to quantify mixing in models. The entropy may be used to analyse the mixed state of the mantle as a whole and may also be useful to validate numerical models against anomalies in the mantle that are obtained from seismology and geochemistry.
Geodynamic models of mantle convection provide a powerful tool to study the structure and...