Deformation experiments conducted in a gas medium apparatus at temperatures from 1200 to 1350°C with a fine-grained, solution-gelation derived Fe-bearing olivine show a stress dependence of the strain rate at stresses above ∼150 MPa, which is much str
High-temperature, high-pressure triaxial compressive creep experiments were carried out on polycryst...
The strength of the lithosphere is typically modelled based on constitutive equations for steady-sta...
The strength of the lithosphere is typically modelled based on constitutive equations for steady-sta...
International audienceWe study the mechanical response and correlated microstructure of axial deform...
Deformation experiments were conducted on fine-grained (3-6 μm), fully synthetic Fo90 olivine aggreg...
International audienceAggregates composed of olivine and magnesiowüstite have been deformed to large...
Although microstructural evolution is critical to strain-dependent processes in Earth's mantle, flow...
Although microstructural evolution is critical to strain-dependent processes in Earth's mantle, flow...
International audienceWe have performed tri-axial compression experiments on olivine aggregates at 9...
Changes in stress applied to mantle rocks, such as those imposed by earthquakes, commonly induce a p...
International audienceRheological properties of mantle minerals and rocks at temperatures (T) approp...
International audiencePolycrystalline samples of San Carlos olivine were deformed at high-pressure (...
The strength of the lithosphere is typically modelled based on constitutive equations for steady-sta...
The strength of the lithosphere is typically modelled based on constitutive equations for steady-sta...
The strength of the lithosphere is typically modelled based on constitutive equations for steady-sta...
High-temperature, high-pressure triaxial compressive creep experiments were carried out on polycryst...
The strength of the lithosphere is typically modelled based on constitutive equations for steady-sta...
The strength of the lithosphere is typically modelled based on constitutive equations for steady-sta...
International audienceWe study the mechanical response and correlated microstructure of axial deform...
Deformation experiments were conducted on fine-grained (3-6 μm), fully synthetic Fo90 olivine aggreg...
International audienceAggregates composed of olivine and magnesiowüstite have been deformed to large...
Although microstructural evolution is critical to strain-dependent processes in Earth's mantle, flow...
Although microstructural evolution is critical to strain-dependent processes in Earth's mantle, flow...
International audienceWe have performed tri-axial compression experiments on olivine aggregates at 9...
Changes in stress applied to mantle rocks, such as those imposed by earthquakes, commonly induce a p...
International audienceRheological properties of mantle minerals and rocks at temperatures (T) approp...
International audiencePolycrystalline samples of San Carlos olivine were deformed at high-pressure (...
The strength of the lithosphere is typically modelled based on constitutive equations for steady-sta...
The strength of the lithosphere is typically modelled based on constitutive equations for steady-sta...
The strength of the lithosphere is typically modelled based on constitutive equations for steady-sta...
High-temperature, high-pressure triaxial compressive creep experiments were carried out on polycryst...
The strength of the lithosphere is typically modelled based on constitutive equations for steady-sta...
The strength of the lithosphere is typically modelled based on constitutive equations for steady-sta...