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Evidence of denser MgSiO(3) glass above 133 gigapascal (GPa) and implications for remnants of ultradense silicate melt from a deep magma ocean
Ultralow velocity zones are the largest seismic anomalies in the mantle, with 10–30% seismic velocity reduction observed in thin layers less than 20–40 km thick, just above the Earth’s core-mantle boundary (CMB). The presence of silicate melts, possibly a remnant of a deep magma ocean in the early E...
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| 主要な著者: | , |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
National Academy of Sciences
2011
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3198344/ https://ncbi.nlm.nih.gov/pubmed/21969547 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1109748108 |
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