Oxidized iron in garnets from the mantle transition zone
The oxidation state of iron in Earth’s mantle is well known to depths of approximately 200 km, but has not been characterized in samples from the lowermost upper mantle (200–410 km depth) or the transition zone (410–660 km depth). Natural samples from the deep (>200 km) mantle are extremely r...
| Main Authors: | , , , , , , , , , , |
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| Format: | Journal article |
| Published: |
Springer Nature
2018
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