AAAAAA

   
Results: 1-10 |
Results: 10
Order-disorder in clay mineral structures
Authors: Plancon, A
Citation: A. Plancon, Order-disorder in clay mineral structures, CLAY MINER, 36(1), 2001, pp. 1-14
Studies of the dehydroxylated-rehydroxylated montmorillonite: Structure ofthe layers and intercalation of water molecules
Authors: Muller, F Plancon, A Drits, VA
Citation: F. Muller et al., Studies of the dehydroxylated-rehydroxylated montmorillonite: Structure ofthe layers and intercalation of water molecules, J PHYS IV, 10(P10), 2000, pp. 481-487
Structural evolution of nacrite as a function of the nature of intercalated organic molecules
Authors: Amara, AB Ben Rhaiem, H Plancon, A
Citation: Ab. Amara et al., Structural evolution of nacrite as a function of the nature of intercalated organic molecules, J APPL CRYS, 33, 2000, pp. 1351-1359
Structural study of a 10 angstrom unstable kaolinite hydrate
Authors: Jemai, S Amara, AB Ben Brahim, J Plancon, A
Citation: S. Jemai et al., Structural study of a 10 angstrom unstable kaolinite hydrate, J APPL CRYS, 33, 2000, pp. 1075-1081
Structural transformation of 2 : 1 dioctahedral layer silicates during dehydroxylation-rehydroxylation reactions
Authors: Muller, F Drits, V Plancon, A Robert, JL
Citation: F. Muller et al., Structural transformation of 2 : 1 dioctahedral layer silicates during dehydroxylation-rehydroxylation reactions, CLAY CLAY M, 48(5), 2000, pp. 572-585
Phase analysis of clays using an expert system and calculation programs for X-ray diffraction by two- and three-component mixed-layer minerals
Authors: Plancon, A Drits, VA
Citation: A. Plancon et Va. Drits, Phase analysis of clays using an expert system and calculation programs for X-ray diffraction by two- and three-component mixed-layer minerals, CLAY CLAY M, 48(1), 2000, pp. 57-62
Dehydroxylation of Fe3+, Mg-rich dioctahedral micas: (I) structural transformation
Authors: Muller, F Drits, VA Plancon, A Besson, G
Citation: F. Muller et al., Dehydroxylation of Fe3+, Mg-rich dioctahedral micas: (I) structural transformation, CLAY MINER, 35(3), 2000, pp. 491-504
Dehydroxylation of Fe3+, Mg-rich dioctahedral micas: (II) cation migration
Authors: Muller, F Drits, VA Tsipursky, SI Plancon, A
Citation: F. Muller et al., Dehydroxylation of Fe3+, Mg-rich dioctahedral micas: (II) cation migration, CLAY MINER, 35(3), 2000, pp. 505-514
An X-ray diffraction study of two hydrated kaolinites, characterized by 10and 8.4 angstrom basal distances, is reported. The study is based on a comparison between the experimental and calculated profiles
Authors: Jemai, S Amara, AB Ben Brahim, J Plancon, A
Citation: S. Jemai et al., An X-ray diffraction study of two hydrated kaolinites, characterized by 10and 8.4 angstrom basal distances, is reported. The study is based on a comparison between the experimental and calculated profiles, J APPL CRYS, 32, 1999, pp. 968-976
Modelisation of X-ray powder diffraction patterns for the study of heat-treated Fe-rich dioctahedral 2 : 1 layer silicates
Authors: Muller, F Plancon, A Drits, VA Besson, G
Citation: F. Muller et al., Modelisation of X-ray powder diffraction patterns for the study of heat-treated Fe-rich dioctahedral 2 : 1 layer silicates, J PHYS IV, 8(P5), 1998, pp. 91-98
Risultati: 1-10 |