Muscovite-2M(1) shows a major phase transition at about 800 degrees C, which is generally attributed in the literature to the structural dehydroxylation process, although a number of structural models have been proposed for the dehydroxylated phase, and different transformation mechanisms have also been put forward. The observed first order transformation involves an increase in the cell volume, and it is not clear to date how the cell expansion is related to the loss of hydroxyl groups. The phase change has been re-investigated here by in situ high temperature powder diffraction, both in non-isothermal and isothermal modes, to combine for the first time the structural and the kinetic interpretation of the transformation. The results unequi...
The dehydroxylation reactions of chrysotile Mg3Si2O5(OH)4 and brucite Mg(OH)2 were studied under ine...
The high-temperature (HT) behaviour of a sample of natural alunite was investigated by means of in s...
Mullite (Mul) formation after high-T muscovite (Ms) breakdown has been studied in phyllosilicate-ric...
Muscovite-2M(1) shows a major phase transition at about 800 degrees C, which is generally attributed...
The high temperature phase transition of muscovite-2M(1) was investigated by "in situ" isothermal Xr...
The high temperature phase transition of muscovite-2M1 was investigated by "in situ" isothermal X-ra...
Dehydroxylation in aluminous dioctahedral 2 :1 layer silicates may be described at the atomic level ...
Phengite samples (2M 1 and 3T politypes) and a synthetic end-member muscovite specimen were studied ...
The kinetics of the dehydroxylation of chrysotile was followed in situ at high temperature using rea...
Abstract: X-ray powder diffraction was used for the study of structural transformations of dioctahed...
X-ray powder diffraction was used for the study of structural transformations of dioctahedral Al-ric...
Celadonite and glauconite samples heated at different temperatures were studied by X-ray and electro...
Synchrotron radiation XRPD is a powerful tool for the in situ investigation of phase transformation ...
The `in situ' thermal behaviour of muscovite-2M1 in the range 25-1300 °C has been studied by high te...
The thermal transformation, stability field, and reaction kinetics of serpentine minerals (antigorit...
The dehydroxylation reactions of chrysotile Mg3Si2O5(OH)4 and brucite Mg(OH)2 were studied under ine...
The high-temperature (HT) behaviour of a sample of natural alunite was investigated by means of in s...
Mullite (Mul) formation after high-T muscovite (Ms) breakdown has been studied in phyllosilicate-ric...
Muscovite-2M(1) shows a major phase transition at about 800 degrees C, which is generally attributed...
The high temperature phase transition of muscovite-2M(1) was investigated by "in situ" isothermal Xr...
The high temperature phase transition of muscovite-2M1 was investigated by "in situ" isothermal X-ra...
Dehydroxylation in aluminous dioctahedral 2 :1 layer silicates may be described at the atomic level ...
Phengite samples (2M 1 and 3T politypes) and a synthetic end-member muscovite specimen were studied ...
The kinetics of the dehydroxylation of chrysotile was followed in situ at high temperature using rea...
Abstract: X-ray powder diffraction was used for the study of structural transformations of dioctahed...
X-ray powder diffraction was used for the study of structural transformations of dioctahedral Al-ric...
Celadonite and glauconite samples heated at different temperatures were studied by X-ray and electro...
Synchrotron radiation XRPD is a powerful tool for the in situ investigation of phase transformation ...
The `in situ' thermal behaviour of muscovite-2M1 in the range 25-1300 °C has been studied by high te...
The thermal transformation, stability field, and reaction kinetics of serpentine minerals (antigorit...
The dehydroxylation reactions of chrysotile Mg3Si2O5(OH)4 and brucite Mg(OH)2 were studied under ine...
The high-temperature (HT) behaviour of a sample of natural alunite was investigated by means of in s...
Mullite (Mul) formation after high-T muscovite (Ms) breakdown has been studied in phyllosilicate-ric...