Synchrotron X-ray analysis of norbergite, Mg2.98Fe0.01Ti0.02Si0.99O4(OH0.31F1.69) structure at high pressure up to 8.2 GPa
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,General Materials Science
Link
http://link.springer.com/content/pdf/10.1007/s00269-008-0248-0.pdf
Reference38 articles.
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2. Crichton WA, Ross NL (2002) Equation of state of dense hydrous magnesium silicate phase A, Mg7Si2O8(OH)6. Am Mineral 87:333–338
3. Crichton WA, Ross NL (2005) Equation of state of dense hydrous magnesium silicates: results from single-crystal X-ray diffraction. Mineral Mag 69:273–287. doi: 10.1180/0026461056930250
4. Crichton WA, Ross NL, Gasparik T (1999) Equation states of magnesium silicates anhydrous B and superhydrous B. Phys Chem Miner 26:570–575. doi: 10.1007/s002690050220
5. Downs RT, Zha C-S, Duffy TS, Finger LW (1996) The equation state of forsterite to 17.2 GPa and effects of pressure media. Am Mineral 81:51–55
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