Department of Earth Sciences, Utrecht University, Princetonlaan 8A, 3584 CB Utrecht, the Netherlands
Viewed
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: 1,138 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
905
192
41
1,138
50
91
HTML: 905
PDF: 192
XML: 41
Total: 1,138
BibTeX: 50
EndNote: 91
Views and downloads (calculated since 12 Dec 2023)
Cumulative views and downloads
(calculated since 12 Dec 2023)
Total article views: 922 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
690
192
40
922
50
91
HTML: 690
PDF: 192
XML: 40
Total: 922
BibTeX: 50
EndNote: 91
Views and downloads (calculated since 19 Jul 2024)
Cumulative views and downloads
(calculated since 19 Jul 2024)
Total article views: 216 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
215
0
1
216
0
0
HTML: 215
PDF: 0
XML: 1
Total: 216
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: 1,138 (including HTML, PDF, and XML)
Thereof 1,106 with geography defined
and 32 with unknown origin.
Total article views: 922 (including HTML, PDF, and XML)
Thereof 902 with geography defined
and 20 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...