Chromium-for-Aluminum Substitution in Synthetic Serpentine
Cr-bearing clay minerals are products of hydrothermal alteration and fluid–rock interactions of ultramafic rocks that form serpentine minerals. Cr is typically observed to substitute for Al in serpentine minerals, but the crystal chemistry and environmental constraints on this substitution are unkno...
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| Главные авторы: | , , |
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| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
MDPI AG
2026-04-01
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| Серии: | Nanomaterials |
| Предметы: | |
| Online-ссылка: | https://www.mdpi.com/2079-4991/16/8/448 |
| Метки: |
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