Multiple seismic reflectors in Earth's lowermost mantle
The modern view of Earth’s lowermost mantle considers a D″ region of enhanced (seismologically inferred) heterogeneity bounded by the core–mantle boundary and an interface some 150–300 km above it, with the latter often attributed to the postperovskite phase transition (in MgSiO[subscript 3]). Seism...
| Главные авторы: | , , , |
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| Другие авторы: | |
| Формат: | Статья |
| Язык: | en_US |
| Опубликовано: |
National Academy of Sciences (U.S.)
2014
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| Online-ссылка: | http://hdl.handle.net/1721.1/90329 https://orcid.org/0000-0003-1650-6818 |