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Multiscale modeling of upper mantle plasticity: From single-crystal rheology to multiphase aggregate deformation

Raterron, Paul; Detrez, Fabrice; Castelnau, Olivier; et al.

Physics of the Earth and Planetary Interiors, 2014, 228, 232-243

Article dans une revue scientifique

Polycrystalline olivine rheology in dislocation creep: Revisiting experimental data to 8.1GPa

Bollinger, Caroline; Raterron, Paul; Cordier, Patrick; et al.

Physics of the Earth and Planetary Interiors, 2014, 228, 211-219

Article dans une revue scientifique

Transmission electron microscopy characterization of dislocations and slip systems in K-lingunite: Implications for the seismic anisotropy of subducted crust

Mussi, Alexandre; Cordier, Patrick; Mainprice, David; et al.

Physics of the Earth and Planetary Interiors, 2010, 182, 50-58

Article dans une revue scientifique

Origin of twist in "gwindel" quartz crystals from the Alps: a transmission electron microscopy study

Cordier, Patrick; Heidelbach, Florian

European Journal of Mineralogy, 2013, 25, 145-153

Article dans une revue scientifique

Low strength of Earth's uppermost mantle inferred from tri-axial deformation experiments on dry olivine crystals

Demouchy, Sylvie; Tommasi, Andréa; Boffa Ballaran, Tiziana; et al.

Physics of the Earth and Planetary Interiors, 2013, 220, 37-49

Article dans une revue scientifique

Deformation of forsterite polycrystals at mantle pressure: Comparison with Fe-bearing olivine and the effect of iron on its plasticity

Bollinger, Caroline; Merkel, Sébastien; Cordier, Patrick; et al.

Physics of the Earth and Planetary Interiors, 2015, 240, 95-104

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Numerical modeling of the core structure of [100] dislocations in Fe3C cementite

Garvik, N.; Carrez, Philippe; Garruchet, S.; et al.

Scripta Materialia, 2015, 99, 61-64

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The formation of nuggets of highly siderophile elements in quenched silicate melts at high temperatures: Before or during the silicate quench?

Malavergne, Valérie; Charon, Emeline; Jones, J.; et al.

Earth and Planetary Science Letters, 2016, 434, 197-207

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Olivine, and the Origin of Kimberlite

How Mercury can be the most reduced terrestrial planet and still store iron in its mantle

Multiscale modeling of upper mantle plasticity: From single-crystal rheology to multiphase aggregate deformation

Polycrystalline olivine rheology in dislocation creep: Revisiting experimental data to 8.1GPa

Transmission electron microscopy characterization of dislocations and slip systems in K-lingunite: Implications for the seismic anisotropy of subducted crust

Origin of twist in "gwindel" quartz crystals from the Alps: a transmission electron microscopy study

Low strength of Earth's uppermost mantle inferred from tri-axial deformation experiments on dry olivine crystals

Deformation of forsterite polycrystals at mantle pressure: Comparison with Fe-bearing olivine and the effect of iron on its plasticity

Numerical modeling of the core structure of [100] dislocations in Fe3C cementite

The formation of nuggets of highly siderophile elements in quenched silicate melts at high temperatures: Before or during the silicate quench?

Search

Olivine, and the Origin of Kimberlite

How Mercury can be the most reduced terrestrial planet and still store iron in its mantle

Multiscale modeling of upper mantle plasticity: From single-crystal rheology to multiphase aggregate deformation

Polycrystalline olivine rheology in dislocation creep: Revisiting experimental data to 8.1GPa

Transmission electron microscopy characterization of dislocations and slip systems in K-lingunite: Implications for the seismic anisotropy of subducted crust

Origin of twist in &quot;gwindel&quot; quartz crystals from the Alps: a transmission electron microscopy study

Low strength of Earth's uppermost mantle inferred from tri-axial deformation experiments on dry olivine crystals

Deformation of forsterite polycrystals at mantle pressure: Comparison with Fe-bearing olivine and the effect of iron on its plasticity

Numerical modeling of the core structure of [100] dislocations in Fe3C cementite

The formation of nuggets of highly siderophile elements in quenched silicate melts at high temperatures: Before or during the silicate quench?

Origin of twist in "gwindel" quartz crystals from the Alps: a transmission electron microscopy study