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Stebbins, J. F., Smyth, J. R., Panero, W. R., Frost, D. J. (2009) Forsterite, hydrous and anhydrous wadsleyite and ringwoodite (Mg2SiO4): 29Si NMR results for chemical shift anisotropy, spin-lattice relaxation, and mechanism of hydration. American Mineralogist, 94 (7) 905-915 doi:10.2138/am.2009.3184

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Reference TypeJournal (article/letter/editorial)
TitleForsterite, hydrous and anhydrous wadsleyite and ringwoodite (Mg2SiO4): 29Si NMR results for chemical shift anisotropy, spin-lattice relaxation, and mechanism of hydration
JournalAmerican Mineralogist
AuthorsStebbins, J. F.Author
Smyth, J. R.Author
Panero, W. R.Author
Frost, D. J.Author
Year2009 (July 1)Volume94
Issue7
PublisherMineralogical Society of America
DOIdoi:10.2138/am.2009.3184Search in ResearchGate
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Mindat Ref. ID396313Long-form Identifiermindat:1:5:396313:9
GUID0
Full ReferenceStebbins, J. F., Smyth, J. R., Panero, W. R., Frost, D. J. (2009) Forsterite, hydrous and anhydrous wadsleyite and ringwoodite (Mg2SiO4): 29Si NMR results for chemical shift anisotropy, spin-lattice relaxation, and mechanism of hydration. American Mineralogist, 94 (7) 905-915 doi:10.2138/am.2009.3184
Plain TextStebbins, J. F., Smyth, J. R., Panero, W. R., Frost, D. J. (2009) Forsterite, hydrous and anhydrous wadsleyite and ringwoodite (Mg2SiO4): 29Si NMR results for chemical shift anisotropy, spin-lattice relaxation, and mechanism of hydration. American Mineralogist, 94 (7) 905-915 doi:10.2138/am.2009.3184
In(2009, July) American Mineralogist Vol. 94 (7) Mineralogical Society of America

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Stebbins, J. F., Panero, W. R., Smyth, J. R., Frost, D. J. (2009) Forsterite, wadsleyite, and ringwoodite (Mg2SiO4): 29Si NMR constraints on structural disorder and effects of paramagnetic impurity ions. American Mineralogist, 94 (4) 626-629 doi:10.2138/am.2009.3140
Ye, Y., Schwering, R. A., Smyth, J. R. (2009) Effects of hydration on thermal expansion of forsterite, wadsleyite, and ringwoodite at ambient pressure. American Mineralogist, 94 (7) 899-904 doi:10.2138/am.2009.3122
Panero, W. R., Smyth, J. R., Pigott, J. S., Liu, Z., Frost, D. J. (2013) Hydrous ringwoodite to 5 K and 35 GPa: Multiple hydrogen bonding sites resolved with FTIR spectroscopy. American Mineralogist, 98 (4) 637-642 doi:10.2138/am.2013.3978
Holl, C. M.; Smyth, J. R.; Jacobsen, S. D.; Frost, D. J. (2008) Effects of hydration on the structure and compressibility of wadsleyite, β-(Mg2SiO4). American Mineralogist, 93 (4). 598-607 doi:10.2138/am.2008.2620
Ashbrook, S. E. (2005) High-resolution 17O MAS NMR spectroscopy of forsterite ( -Mg2SiO4), wadsleyite ( -Mg2SiO4), and ringwoodite ( -Mg2SiO4) American Mineralogist, 90 (11) 1861-1870 doi:10.2138/am.2005.1915
Hushur, A., Manghnani, M. H., Smyth, J. R., Nestola, F., Frost, D. J. (2009) Crystal chemistry of hydrous forsterite and its vibrational properties up to 41 GPa. American Mineralogist, 94 (5) 751-760 doi:10.2138/am.2009.2990
Ye, Y., Brown, D. A., Smyth, J. R., Panero, W. R., Jacobsen, S. D., Chang, Y.-Y., Townsend, J. P., Thomas, S.-M., Hauri, E. H., Dera, P., Frost, D. J. (2012) Compressibility and thermal expansion of hydrous ringwoodite with 2.5(3) wt% H2O. American Mineralogist, 97 (4) 573-582 doi:10.2138/am.2012.4010
Trots, D. M., Kurnosov, A., Ballaran, T. B., Frost, D. J. (2012) High-temperature structural behaviors of anhydrous wadsleyite and forsterite. American Mineralogist, 97 (10) 1582-1590 doi:10.2138/am.2012.3992
Ye, Y., Smyth, J. R., Hushur, A., Manghnani, M. H., Lonappan, D., Dera, P., Frost, D. J. (2010) Crystal structure of hydrous wadsleyite with 2.8% H2O and compressibility to 60 GPa. American Mineralogist, 95 (11) 1765-1772 doi:10.2138/am.2010.3533
Ye, Y., Smyth, J. R., Frost, D. J. (2011) Structural study of the coherent dehydration of wadsleyite. American Mineralogist, 96 (11) 1760-1767 doi:10.2138/am.2011.3852
Smyth, Joseph R., Holl, Christopher M., Frost, Daniel J., Jacobsen, Steven D., Langenhorst, Falko, Mccammon, Catherine A. (2003) Structural systematics of hydrous ringwoodite and water in Earth’s interior. American Mineralogist, 88 (10) 1402-1407 doi:10.2138/am-2003-1001
 
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