Abstract
An idea that a mineral phase transition may occur not once, but twice, close to the core-mantle boundary has been tested with seismic data. The resulting picture of the deep Earth is sure to provoke debate.
| Original language | English |
|---|---|
| Pages (from-to) | 834-835 |
| Number of pages | 2 |
| Journal | Nature |
| Volume | 434 |
| Issue number | 7035 |
| DOIs | |
| State | Published - Apr 14 2005 |
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