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Global geochemical fingerprinting of plume intensity suggests coupling with the supercontinent cycle
Plate tectonics and mantle plumes are two of the most fundamental solid-Earth processes that have operated through much of Earth history. For the past 300 million years, mantle plumes are known to derive mostly from two large low shear velocity provinces (LLSVPs) above the core-mantle boundary, refe...
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| Vydáno v: | Nat Commun |
|---|---|
| Hlavní autoři: | , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2019
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6872659/ https://ncbi.nlm.nih.gov/pubmed/31754134 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-13300-4 |
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