Seismic discontinuities and subduction zones
The seismic discontinuities at 410 and 660 km depth in the mantle are generally believed to be due to phase transformations in its major component, olivine. An increasing observational base of short-period regional seismic network data supports this view. Here, we analyse cross-sections of discontin...
| Автори: | , , |
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| Формат: | Conference item |
| Опубліковано: |
2001
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