Department of Earth Sciences, Utrecht University, Princetonlaan 8A, 3584 CB Utrecht, the Netherlands
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Total article views: 2,941 (including HTML, PDF, and XML)
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2,152
631
158
2,941
142
189
HTML: 2,152
PDF: 631
XML: 158
Total: 2,941
BibTeX: 142
EndNote: 189
Views and downloads (calculated since 12 Dec 2023)
Cumulative views and downloads
(calculated since 12 Dec 2023)
Total article views: 1,989 (including HTML, PDF, and XML)
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XML
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BibTeX
EndNote
1,210
631
148
1,989
142
189
HTML: 1,210
PDF: 631
XML: 148
Total: 1,989
BibTeX: 142
EndNote: 189
Views and downloads (calculated since 19 Jul 2024)
Cumulative views and downloads
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Total article views: 952 (including HTML, PDF, and XML)
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942
0
10
952
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HTML: 942
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Total: 952
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: 2,941 (including HTML, PDF, and XML)
Thereof 2,852 with geography defined
and 89 with unknown origin.
Total article views: 1,989 (including HTML, PDF, and XML)
Thereof 1,912 with geography defined
and 77 with unknown origin.
Total article views: 952 (including HTML, PDF, and XML)
Thereof 940 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...