Department of Earth Sciences, Utrecht University, Princetonlaan 8A, 3584 CB Utrecht, the Netherlands
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Total article views: 2,630 (including HTML, PDF, and XML)
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1,962
562
106
2,630
98
141
HTML: 1,962
PDF: 562
XML: 106
Total: 2,630
BibTeX: 98
EndNote: 141
Views and downloads (calculated since 12 Dec 2023)
Cumulative views and downloads
(calculated since 12 Dec 2023)
Total article views: 1,692 (including HTML, PDF, and XML)
HTML
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XML
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1,033
562
97
1,692
98
141
HTML: 1,033
PDF: 562
XML: 97
Total: 1,692
BibTeX: 98
EndNote: 141
Views and downloads (calculated since 19 Jul 2024)
Cumulative views and downloads
(calculated since 19 Jul 2024)
Total article views: 938 (including HTML, PDF, and XML)
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929
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9
938
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Total: 938
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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: 2,630 (including HTML, PDF, and XML)
Thereof 2,552 with geography defined
and 78 with unknown origin.
Total article views: 1,692 (including HTML, PDF, and XML)
Thereof 1,626 with geography defined
and 66 with unknown origin.
Total article views: 938 (including HTML, PDF, and XML)
Thereof 926 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...