Defects in olivine
<p>Olivine, a ferromagnesian orthosilicate, is the most abundant mineral in Earth's upper mantle and is stable down to the olivine–wadsleyite phase transition, which defines the 410 km depth mantle transition zone. Olivine also occurs in crustal environments in metamorphic and hydrotherma...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2021-05-01
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| Series: | European Journal of Mineralogy |
| Online Access: | https://ejm.copernicus.org/articles/33/249/2021/ejm-33-249-2021.pdf |