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: 2,651 (including HTML, PDF, and XML)
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1,969
572
110
2,651
100
143
HTML: 1,969
PDF: 572
XML: 110
Total: 2,651
BibTeX: 100
EndNote: 143
Views and downloads (calculated since 12 Dec 2023)
Cumulative views and downloads
(calculated since 12 Dec 2023)
Total article views: 1,712 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,040
572
100
1,712
100
143
HTML: 1,040
PDF: 572
XML: 100
Total: 1,712
BibTeX: 100
EndNote: 143
Views and downloads (calculated since 19 Jul 2024)
Cumulative views and downloads
(calculated since 19 Jul 2024)
Total article views: 939 (including HTML, PDF, and XML)
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929
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10
939
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XML: 10
Total: 939
BibTeX: 0
EndNote: 0
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: 2,651 (including HTML, PDF, and XML)
Thereof 2,572 with geography defined
and 79 with unknown origin.
Total article views: 1,712 (including HTML, PDF, and XML)
Thereof 1,645 with geography defined
and 67 with unknown origin.
Total article views: 939 (including HTML, PDF, and XML)
Thereof 927 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...