Hidden Oceans? Unraveling the Structure of Hydrous Defects in the Earth’s Deep Interior
High-pressure silicates making up the main proportion of the earth’s interior can incorporate a significant amount of water in the form of OH defects. Generally, they are charge balanced by removing low-valent cations such as Mg2+. By combining high-resolution multidimensional single- and double-qua...
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Veröffentlicht in: | Journal of the American Chemical Society 2017-08, Vol.139 (30), p.10499-10505 |
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Format: | Artikel |
Sprache: | eng |
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