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Coupled dynamics and evolution of primordial and recycled heterogeneity in Earth's lower mantle - Supplementary Videos

Anna J. P. Gülcher


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    "description": "<p><strong>Supplementary Videos</strong></p>\n\n<p>This .zip folder contains all Supplementary Videos related to the preprint &quot;Coupled dynamics and evolution of primordial and recycled heterogeneity in Earth&#39;s lower mantle&quot; by G&uuml;lcher et al. (<em>submitted to EGU Solid Earth</em>). Each regime discussed in this paper has been represented by a selected numerical model, displayed in all of the figures. For each of them, a video has been made showing the evolution through time of the primordial composition field as well as the potential temperature field. For the discussion of the evolution of these models, the reader is referred to the paper.</p>\n\n<p>&nbsp;</p>\n\n<p><strong>Supplementary video 1 &ndash;&nbsp;</strong>evolution of Model&nbsp;<strong>M</strong><strong><sub>100k&nbsp;</sub></strong>(<em>D</em><sub>prim&nbsp;</sub>= 2230 km,&nbsp;<span class=\"math-tex\">\\(\\lambda\\)</span><sub>prim</sub>= 100 and&nbsp;<em>B</em>= 0.78;&nbsp;<strong>regime&nbsp;</strong><strong>II.T</strong>)</p>\n\n<p><strong>Supplementary video 2 -&nbsp;</strong>evolution of Model&nbsp;<strong>M<sub>10b&nbsp;</sub></strong>(<em>D</em><sub>prim&nbsp;</sub>= 2230 km,&nbsp;&nbsp;<span class=\"math-tex\">\\(\\lambda\\)</span><sub>prim</sub>= 10 and&nbsp;<em>B</em>= 0.14;&nbsp;<strong>regime&nbsp;</strong><strong>II.R<sub>S</sub></strong>)</p>\n\n<p><strong>Supplementary video 3 -&nbsp;</strong>evolution of Model&nbsp;<strong>M</strong><strong><sub>50a&nbsp;</sub></strong>(<em>D</em><sub>prim&nbsp;</sub>= 2230 km,&nbsp;&nbsp;<span class=\"math-tex\">\\(\\lambda\\)</span><sub>prim</sub>= 50 and&nbsp;<em>B</em>= 0.07;&nbsp;<strong>regime&nbsp;</strong><strong>II.R<sub>E</sub></strong>)</p>\n\n<p><strong>Supplementary video 4 -&nbsp;</strong>evolution of Model&nbsp;<strong>M</strong><strong><sub>300i&nbsp;</sub></strong>(<em>D</em><sub>prim&nbsp;</sub>= 2230 km,&nbsp;&nbsp;<span class=\"math-tex\">\\(\\lambda\\)</span><sub>prim</sub>= 300 and&nbsp;<em>B</em>= 0.64;&nbsp;<strong>regime&nbsp;</strong><strong>III.P</strong>)</p>\n\n<p><strong>Supplementary video 5 -&nbsp;</strong>evolution of Model&nbsp;<strong>M</strong><strong><sub>300d&nbsp;</sub></strong>(<em>D</em><sub>prim&nbsp;</sub>= 2230 km,&nbsp;&nbsp;<span class=\"math-tex\">\\(\\lambda\\)</span><sub>prim</sub>= 300 and&nbsp;<em>B</em>= 0.28;&nbsp;<strong>regime&nbsp;</strong><strong>III.B</strong>)</p>\n\n<p><strong>Supplementary video 6 -&nbsp;</strong>evolution of Model&nbsp;<strong>M</strong><strong><sub>100d&nbsp;</sub></strong>(<em>D</em><sub>prim&nbsp;</sub>= 2230 km,&nbsp;&nbsp;<span class=\"math-tex\">\\(\\lambda\\)</span><sub>prim</sub>= 100 and&nbsp;<em>B</em>= 0.28;&nbsp;<strong>regime&nbsp;</strong><strong>III.B</strong>)</p>\n\n<p><strong>Supplementary video 7 -&nbsp;</strong>evolution of Model&nbsp;<strong>M</strong><strong><sub>30c&nbsp;</sub></strong>(<em>D</em><sub>prim&nbsp;</sub>= 2230 km,&nbsp;&nbsp;<span class=\"math-tex\">\\(\\lambda\\)</span><sub>prim</sub>= 30 and&nbsp;<em>B</em>= 0.21;&nbsp;<strong>regime&nbsp;</strong><strong>III.M</strong>)</p>\n\n<p><strong>Supplementary video 8 -&nbsp;</strong>evolution of Model&nbsp;<strong>M</strong><strong><sub>10f&nbsp;</sub></strong>(<em>D</em><sub>prim&nbsp;</sub>= 2230 km,&nbsp;&nbsp;<span class=\"math-tex\">\\(\\lambda\\)</span><sub>prim</sub>= 10 and&nbsp;<em>B</em>= 0.42;&nbsp;<strong>regime&nbsp;</strong><strong>III.D</strong>)</p>\n\n<p><strong>Supplementary video 9 -&nbsp;</strong>evolution of Model&nbsp;<strong>M</strong><strong><sub>100dD&nbsp;</sub></strong>(<em>D</em><sub>prim&nbsp;</sub>= 1650 km,&nbsp;&nbsp;<span class=\"math-tex\">\\(\\lambda\\)</span><sub>prim</sub>= 100 and&nbsp;<em>B</em>= 0.28;&nbsp;<strong>regime&nbsp;</strong><strong>III.B</strong>)</p>\n\n<p><strong>Supplementary video 10 -&nbsp;</strong>evolution of Model&nbsp;<strong>M</strong><strong><sub>50eD&nbsp;</sub></strong>(<em>D</em><sub>prim&nbsp;</sub>= 1695 km,&nbsp;&nbsp;<span class=\"math-tex\">\\(\\lambda\\)</span><sub>prim</sub>= 50 and&nbsp;<em>B</em>= 0.35;&nbsp;<strong>regime&nbsp;</strong><strong>III.B</strong>)</p>\n\n<p><strong>Supplementary video 11 -&nbsp;</strong>evolution of Model&nbsp;<strong>M</strong><strong><sub>30cD&nbsp;</sub></strong>(<em>D</em><sub>prim&nbsp;</sub>= 1583 km,&nbsp;&nbsp;<span class=\"math-tex\">\\(\\lambda\\)</span><sub>prim</sub>= 30 and&nbsp;<em>B</em>= 0.21;&nbsp;<strong>regime&nbsp;</strong><strong>III.B</strong>)</p>\n\n<p><strong>Supplementary video 12 -&nbsp;</strong>evolution of Model&nbsp;<strong>M<sup>B1</sup></strong><strong><sub>100dD&nbsp;</sub></strong>(<em>D</em><sub>FeO-rich_layer&nbsp;</sub>= 200 km, <em>D</em><sub>prim&nbsp;</sub>= 1546 km,&nbsp;&nbsp;<span class=\"math-tex\">\\(\\lambda\\)</span><sub>prim</sub>= 100 and&nbsp;<em>B</em>= 0.28;&nbsp;<strong>regime&nbsp;</strong><strong>III.B</strong>)</p>", 
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