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Mantle rocks shallower than about 410 km depth consist mostly of olivine, pyroxenes, spinel-structure minerals, and garnet.

These mionerals make up rocks called peridotite, dunite (olivine-rich peridotite), and eclogite. We know these from xenoliths brought up with magmas.

Between 410 km and 650 km, olivine is no longer stable and is replaced by its polymorphs wadsleyite and ringwoodite.

Below about 650 km, all of the minerals of the upper mantle begin to become unstable due to the extreme pressure and elevated temperatures. It is difficult for us to know which minerals will be stable in these conditions but we believe silicate perovskites and ferropericlase will prediminate (and diamond).

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11y ago
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Q: What minerals comprise the rocks of Earth's mantle?
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