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A Multi-Technique Characterization of Cronstedtite Synthesized by Iron-Clay Interaction in a Step-By-Step Cooling Procedure
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- Journal:
- Clays and Clay Minerals / Volume 61 / Issue 4 / August 2013
- Published online by Cambridge University Press:
- 01 January 2024, pp. 277-289
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Experimental alteration of Mg-vermiculite under hydrothermal conditions: formation of mixed-layered saponite-chlorite minerals
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- Journal:
- Clay Minerals / Volume 38 / Issue 3 / September 2003
- Published online by Cambridge University Press:
- 09 July 2018, pp. 303-314
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Experimental synthesis of chlorite from smectite at 300ºC in the presence of metallic Fe
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- Journal:
- Clay Minerals / Volume 38 / Issue 3 / September 2003
- Published online by Cambridge University Press:
- 09 July 2018, pp. 281-302
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Oxidation of mudstone in a tunnel (Tournemire, France): consequences for the mineralogy and crystal chemistry of clay minerals
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- Journal:
- Clay Minerals / Volume 39 / Issue 2 / June 2004
- Published online by Cambridge University Press:
- 09 July 2018, pp. 135-149
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Characterization of smectite and illite by FTIR spectroscopy of interlayer NH4+ cations
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- Journal:
- Clay Minerals / Volume 38 / Issue 2 / June 2003
- Published online by Cambridge University Press:
- 09 July 2018, pp. 201-211
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Experimental study of the transformation of smectite at 80 and 300ºC in the presence of Fe oxides
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- Journal:
- Clay Minerals / Volume 39 / Issue 1 / March 2004
- Published online by Cambridge University Press:
- 09 July 2018, pp. 17-34
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Rythmic changes in crystal chemistry of trioctahedral Cr-chlorites and Cr entrapment: a SEM, EM and Raman study
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- Journal:
- Clay Minerals / Volume 38 / Issue 3 / September 2003
- Published online by Cambridge University Press:
- 09 July 2018, pp. 339-352
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Hydrothermal reactivity of K-smectite at 300°C and 100 bar: dissolution-crystallization process and non-expandable dehydrated smectite formation
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- Journal:
- Clay Minerals / Volume 34 / Issue 2 / June 1999
- Published online by Cambridge University Press:
- 09 July 2018, pp. 275-290
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