Department of Earth Sciences, Utrecht University, Princetonlaan 8A, 3584 CB Utrecht, the Netherlands
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Total article views: 1,013 (including HTML, PDF, and XML)
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824
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33
1,013
36
62
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PDF: 156
XML: 33
Total: 1,013
BibTeX: 36
EndNote: 62
Views and downloads (calculated since 12 Dec 2023)
Cumulative views and downloads
(calculated since 12 Dec 2023)
Total article views: 797 (including HTML, PDF, and XML)
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609
156
32
797
36
62
HTML: 609
PDF: 156
XML: 32
Total: 797
BibTeX: 36
EndNote: 62
Views and downloads (calculated since 19 Jul 2024)
Cumulative views and downloads
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Total article views: 216 (including HTML, PDF, and XML)
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215
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Views and downloads (calculated since 12 Dec 2023)
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: 1,013 (including HTML, PDF, and XML)
Thereof 986 with geography defined
and 27 with unknown origin.
Total article views: 797 (including HTML, PDF, and XML)
Thereof 782 with geography defined
and 15 with unknown origin.
Total article views: 216 (including HTML, PDF, and XML)
Thereof 204 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...