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Ferrage, E., Vidal, O., Mosser-Ruck, R., Cathelineau, M., Cuadros, J. (2011) A reinvestigation of smectite illitization in experimental hydrothermal conditions: Results from X-ray diffraction and transmission electron microscopy. American Mineralogist, 96 (1) 207-223 doi:10.2138/am.2011.3587

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Reference TypeJournal (article/letter/editorial)
TitleA reinvestigation of smectite illitization in experimental hydrothermal conditions: Results from X-ray diffraction and transmission electron microscopy
JournalAmerican Mineralogist
AuthorsFerrage, E.Author
Vidal, O.Author
Mosser-Ruck, R.Author
Cathelineau, M.Author
Cuadros, J.Author
Year2011 (January 1)Volume96
Issue1
PublisherMineralogical Society of America
DOIdoi:10.2138/am.2011.3587Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID396604Long-form Identifiermindat:1:5:396604:8
GUID0
Full ReferenceFerrage, E., Vidal, O., Mosser-Ruck, R., Cathelineau, M., Cuadros, J. (2011) A reinvestigation of smectite illitization in experimental hydrothermal conditions: Results from X-ray diffraction and transmission electron microscopy. American Mineralogist, 96 (1) 207-223 doi:10.2138/am.2011.3587
Plain TextFerrage, E., Vidal, O., Mosser-Ruck, R., Cathelineau, M., Cuadros, J. (2011) A reinvestigation of smectite illitization in experimental hydrothermal conditions: Results from X-ray diffraction and transmission electron microscopy. American Mineralogist, 96 (1) 207-223 doi:10.2138/am.2011.3587
In(2011, January) American Mineralogist Vol. 96 (1) Mineralogical Society of America

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Ferrage, E., Vidal, O., Mosser-Ruck, R., Cathelineau, M. (2011) A reinvestigation of smectite illitization in experimental hydrothermal conditions: Results from X-ray diffraction and transmission electron microscopy--Reply. American Mineralogist, 96 (11) 1903-1904 doi:10.2138/am.2011.3945
Yates, D. M., Rosenberg, P. E. (2011) A reinvestigation of smectite illitization in experimental hydrothermal conditions: Results from X-ray diffraction and transmission electron microscopy--Discussion. American Mineralogist, 96 (11) 1901-1902 doi:10.2138/am.2011.3875
Ferrage, E. (2005) Investigation of smectite hydration properties by modeling experimental X-ray diffraction patterns: Part I. Montmorillonite hydration properties. American Mineralogist, 90 (8) 1358-1374 doi:10.2138/am.2005.1776
Cuadros, J., Dekov, V. M., Fiore, S. (2008) Crystal chemistry of the mixed-layer sequence talc-talc-smectite-smectite from submarine hydrothermal vents. American Mineralogist, 93 (8) 1338-1348 doi:10.2138/am.2008.2692
Mosser-Ruck, Regine, Pironon, Jacques, Cathelineau, Michel, Trouiller, Alain (2001) Experimental illitization of smectite in a K-rich solution. European Journal of Mineralogy, 13 (5) 829-840 doi:10.1127/0935-1221/2001/0013/0829
Mosser-Ruck, R, Cathelineau, M (2004) Experimental transformation of Na,Ca-smectite under basic conditions at 150 °C. Applied Clay Science, 26. 259-273 doi:10.1016/j.clay.2003.12.011
Lopano, C. L., Heaney, P. J., Post, J. E. (2009) Cs-exchange in birnessite: Reaction mechanisms inferred from time-resolved X-ray diffraction and transmission electron microscopy. American Mineralogist, 94 (5) 816-826 doi:10.2138/am.2009.3068
Dazas, B., Ferrage, E., Delville, A., Lanson, B. (2014) Interlayer structure model of tri-hydrated low-charge smectite by X-ray diffraction and Monte Carlo modeling in the Grand Canonical ensemble. American Mineralogist, 99 (8) 1724-1735 doi:10.2138/am.2014.4846
Ferrage, E., Lanson, B., Sakharov, B. A., Geoffroy, N., Jacquot, E., Drits, V. A. (2007) Investigation of dioctahedral smectite hydration properties by modeling of X-ray diffraction profiles: Influence of layer charge and charge location. American Mineralogist, 92 (10) 1731-1743 doi:10.2138/am.2007.2273
Dudek, T., Cuadros, J., Huertas, J. (2007) Structure of mixed-layer kaolinite-smectite and smectite-to-kaolinite transformation mechanism from synthesis experiments. American Mineralogist, 92 (1) 179-192 doi:10.2138/am.2007.2218
Mosser-Ruck, R., Cathelineau, M., Baronnet, A., Trouiller, A. (1999) Hydrothermal reactivity of K-smectite at 300°C and 100 bar: dissolution-crystallization process and non-expandable dehydrated smectite formation. Clay Minerals, 34 (2) 275-290 doi:10.1180/000985599546235
 
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