High-temperature structural disorders stabilize hydrous aluminosilicates in the mantle transition zone.

Nat Commun · 2025 · PMC11762294 · PMID 39863611

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may be significantno p-value reported

Therefore, if high-pressure hydrous minerals can withstand high temperatures in the mantle, the water reservoirs and fluxes may be significant in the Earth’s deep interior.

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