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: 2,700 (including HTML, PDF, and XML)
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EndNote
1,990
598
112
2,700
103
145
HTML: 1,990
PDF: 598
XML: 112
Total: 2,700
BibTeX: 103
EndNote: 145
Views and downloads (calculated since 12 Dec 2023)
Cumulative views and downloads
(calculated since 12 Dec 2023)
Total article views: 1,758 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,058
598
102
1,758
103
145
HTML: 1,058
PDF: 598
XML: 102
Total: 1,758
BibTeX: 103
EndNote: 145
Views and downloads (calculated since 19 Jul 2024)
Cumulative views and downloads
(calculated since 19 Jul 2024)
Total article views: 942 (including HTML, PDF, and XML)
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932
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10
942
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Total: 942
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: 2,700 (including HTML, PDF, and XML)
Thereof 2,616 with geography defined
and 84 with unknown origin.
Total article views: 1,758 (including HTML, PDF, and XML)
Thereof 1,686 with geography defined
and 72 with unknown origin.
Total article views: 942 (including HTML, PDF, and XML)
Thereof 930 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...