Search Results - "Raterron, Paul"
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Polycrystalline olivine rheology in dislocation creep: Revisiting experimental data to 8.1GPa
Published in Physics of the earth and planetary interiors (01-03-2014)“…•Activation enthalpy for olivine polycrystals rheology increases linearly with P.•For olivine polycrystals up to 8.1GPa, V∗=12.8+/− 5cm3mol−1.•Deformation data…”
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Constitutive Law and Flow Mechanism in Diamond Deformation
Published in Scientific reports (19-11-2012)“…Constitutive laws and crystal plasticity in diamond deformation have been the subjects of substantial interest since synthetic diamond was made in 1950's. To…”
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Experimental deformation of olivine single crystals at mantle pressures and temperatures
Published in Physics of the earth and planetary interiors (01-01-2009)“…Deformation experiments were carried out in a deformation-DIA high-pressure apparatus (D-DIA) on oriented San Carlos olivine single crystals, at pressure ( P)…”
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Pressure Dependence of Magnesite Creep
Published in Geosciences (Basel) (01-10-2019)“…We determined the activation volumes (V*) for polycrystalline magnesite with grain sizes of 2 and 80 µm deforming by low temperature plasticity (LTP)…”
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Low-temperature olivine rheology at high pressure
Published in Physics of the earth and planetary interiors (30-07-2004)“…San-Carlos olivine rheology was investigated at pressure ( P) up to 9 GPa and temperature ( T) lower than 890 °C. Six powder specimens were cold compressed and…”
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A process for low-temperature olivine-spinel transition under quasi-hydrostatic stress
Published in Geophysical research letters (15-05-2002)“…The behavior of fayalite—the Fe2SiO4 olivine end‐member (Fa100)—has been monitored during high‐pressure and low‐temperature experiments using in‐situ x‐ray…”
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The Effect of Pressure and Mg‐Content on Ilmenite Rheology: Implications for Lunar Cumulate Mantle Overturn
Published in Journal of geophysical research. Planets (01-01-2021)“…The viscosity of ilmenite is an important parameter that is thought to have influenced the thermal and chemical evolution of the lunar cumulate mantle. We…”
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Strength of orthoenstatite single crystals at mantle pressure and temperature and comparison with olivine
Published in Earth and planetary science letters (15-09-2016)“…Oriented single crystals of orthopyroxenes (OPx) were deformed in axisymmetric compression in the D-DIA at pressure and temperature in excess of 3 GPa and 1040…”
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Deformation of forsterite polycrystals at mantle pressure: Comparison with Fe-bearing olivine and the effect of iron on its plasticity
Published in Physics of the earth and planetary interiors (01-03-2015)“…•Activation enthalpy for forsterite polycrystals rheology increases linearly with P.•For forsterite polycrystals at 1473K and up to 8.1GPa,…”
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Strength of orthoenstatite single crystals at mantle pressure and temperature and comparison with olivine
Published in Earth and planetary science letters (01-09-2016)Get full text
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Pressure effect on forsterite dislocation slip systems: Implications for upper-mantle LPO and low viscosity zone
Published in Physics of the earth and planetary interiors (01-09-2011)“…► Olivine deforms by dislocation creep in the top 200 km of the upper mantle. ► We quantify the effect of pressure on olivine [1 0 0] and [0 0 1] dislocation…”
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Hydrolytic weakening of olivine at mantle pressure: Evidence of [100](010) slip system softening from single-crystal deformation experiments
Published in Physics of the earth and planetary interiors (01-03-2013)“…► We report experimental results on the effect of water on the [100] slip of olivine. ► The weakening factor (σdry/σwet at same strain rate) ranges from 1.3 to…”
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Activities of olivine slip systems in the upper mantle
Published in Physics of the earth and planetary interiors (01-06-2012)“…► Upper mantle thermal convection depends on olivine plasticity at high pressure. ► We investigate experimentally the effect of pressure on dry olivine crystal…”
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Polycrystalline olivine rheology in dislocation creep: Revisiting experimental data to 8.1 GPa
Published in Physics of the earth and planetary interiors (01-03-2014)“…The rheology of polycristalline San Carlos olivine is investigated on synchrotron beamline in the Deformation-DIA (D-DIA) at pressure (P) between 3.8 and 8.1…”
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Textures in deforming forsterite aggregates up to 8 GPa and 1673 K
Published in Physics and chemistry of minerals (01-06-2016)“…We report results from axisymmetric deformation experiments carried out on forsterite aggregates in the deformation-DIA apparatus, at upper mantle pressures…”
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In situ quantitative analysis of stress and texture development in forsterite aggregates deformed at 6 GPa and 1373 K
Published in Journal of applied crystallography (01-04-2012)“…The investigation of materials plastic properties at high pressure is a fast‐growing field, owing to the coupling of high‐pressure deformation apparatuses with…”
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Stress Balance in Synthetic Serpentinized Peridotites Deformed at Subduction Zone Pressures
Published in Journal of geophysical research. Solid earth (01-03-2024)“…Weak serpentine minerals affect the mechanical behavior of serpentinized peridotites at depth, and may play a significant role in deformation localization…”
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Multiscale modeling of upper mantle plasticity: From single-crystal rheology to multiphase aggregate deformation
Published in Physics of the earth and planetary interiors (01-03-2014)“…•We model the plasticity of olivine+diopside aggregates as analogue of peridotite.•The mean-field SO model accounts for an isotropic ‘diffusion-related’…”
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In situ rheological measurements at extreme pressure and temperature using synchrotron X-ray diffraction and radiography
Published in Journal of synchrotron radiation (01-11-2009)“…Dramatic technical progress seen over the past decade now allows the plastic properties of materials to be investigated under extreme pressure and temperature…”
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