Abstract
Magmas that have erupted at Earth's surface reveal a potential new mantle source. This source, which is rich in nickel and has a primordial helium isotopic content, may have originated at great depth in the mantle.
| Original language | English |
|---|---|
| Pages (from-to) | 309-310 |
| Number of pages | 2 |
| Journal | Nature |
| Volume | 493 |
| Issue number | 7432 |
| Publication status | Published - 17 Jan 2013 |
Keywords
- MANTLE
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