Sanchez-Valle C.; Martinez I.; Daniel I.; Philippot P.(2003)
In-situ measurements of the amount of dissolution of carbonate minerals at high pressures (up to 3.6 GPa) and temperatures (up to 523 K) are reported. Using an externally heated diamond anvil cell (DAC) and synchrotron ...
Auzende A.L.; Daniel I.; Reynard B.; Lemaire C.; Guyot F.(2004)
Four main serpentine varieties can be distinguished on the basis of their microstructures, i.e. lizardite, antigorite, chrysotile and polygonal serpentine. Among these, antigorite is the variety stable under high pressure. ...
Perrillat J.P.; Daniel I.; Lardeaux J.M.; Cardon H.(2003)
The kinetics of the quartz–coesite phase transition has been studied in situ by X-ray diffraction in the 2·1–3·2 GPa, 500–1010°C pressure–temperature range. Analysis of the data within Cahn's model of nucleation and growth ...