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Whole-mantle convection with tectonic plates preserves long-term global patterns of upper mantle geochemistry
The evolution of the planetary interior during plate tectonics is controlled by slow convection within the mantle. Global-scale geochemical differences across the upper mantle are known, but how they are preserved during convection has not been adequately explained. We demonstrate that the geographi...
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| Vydáno v: | Sci Rep |
|---|---|
| Hlavní autoři: | , , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2017
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5431867/ https://ncbi.nlm.nih.gov/pubmed/28500352 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-017-01816-y |
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