The crystal structure of the two dense hydrous magnesium silicates Phase D, MgSi2H2O6, and Phase H, MgSiH2O4, synthesized at 45 GPa and 1000 °C and coexisting in the same micrometer-sized grain, was investigated by single-crystal X‑ray diffraction to study the preferential partition of Al between the two structures.
Partition of Al between Phase D and Phase H at high pressure: Results from a simultaneous structure refinement of the two phases coexisting in a unique grain / Bindi, Luca; Nishi, Masayuki; Irifune, Tetsuo. - In: AMERICAN MINERALOGIST. - ISSN 0003-004X. - STAMPA. - 100:(2015), pp. 1637-1640.
Partition of Al between Phase D and Phase H at high pressure: Results from a simultaneous structure refinement of the two phases coexisting in a unique grain
BINDI, LUCA;
2015
Abstract
The crystal structure of the two dense hydrous magnesium silicates Phase D, MgSi2H2O6, and Phase H, MgSiH2O4, synthesized at 45 GPa and 1000 °C and coexisting in the same micrometer-sized grain, was investigated by single-crystal X‑ray diffraction to study the preferential partition of Al between the two structures.
File in questo prodotto:
| File | Dimensione | Formato | |
|---|---|---|---|
|
PhaseD-PhaseH.pdf
Accesso chiuso
Tipologia:
Versione finale referata (Postprint, Accepted manuscript)
Licenza:
Tutti i diritti riservati
Dimensione
688.98 kB
Formato
Adobe PDF
|
688.98 kB | Adobe PDF | Richiedi una copia |
I documenti in FLORE sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
