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Buoyant hydrous mantle plume from the mantle transition zone
Magmatism at some intraplate volcanoes and large igneous provinces (LIPs) in continental areas may originate from hydrous mantle upwelling (i.e. a plume) from the mantle transition zone (MTZ) at 410–660 km depths in the Earth’s deep interior. However, the ultimate origin of the magmatism, i.e. why m...
में बचाया:
| में प्रकाशित: | Sci Rep |
|---|---|
| मुख्य लेखकों: | , , , , , , , , |
| स्वरूप: | Artigo |
| भाषा: | Inglês |
| प्रकाशित: |
Nature Publishing Group UK
2019
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| विषय: | |
| ऑनलाइन पहुंच: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6484022/ https://ncbi.nlm.nih.gov/pubmed/31024064 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-019-43103-y |
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