Physics
Scientist
Géosciences Montpellier, CNRS, Montpellier, France
An in situ trace elements study of serpentinites from the MARK area (ODP site 920, 23°N)
Changes in seal capacity of fractured claystone caprocks induced by dissolved and gaseous CO2 seepage
Erratum to “Relationships between the microstructural evolution and the rheology of talc atelevated pressures and températures” [Earth Planet. Sci. Lett. 268 (2008) 463 475]
Experimental study of carbon sequestration reactions controlled by the percolation of CO2-rich brine through peridotites
Relationships between the microstructural evolution and the rheology of talc at elevated pressures and temperatures
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