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Experimental and observational evidence for plume-induced subduction on Venus

Nature geoscience, 2017-05, Vol.10 (5), p.349-355

2017

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The chemical composition of the Earth: Enstatite chondrite models

Earth and planetary science letters, 2010-05, Vol.293 (3-4), p.259-268

2010

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Formation and Evolution of Protoatmospheres

Space Science Reviews, 2016-12, Vol.205 (1-4), p.153-211

2016

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Thermal evolution of an early magma ocean in interaction with the atmosphere

Journal of geophysical research. Planets, 2013-06, Vol.118 (6), p.1155-1176

2013

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The relative influence of H2O and CO2 on the primitive surface conditions and evolution of rocky planets

Journal of geophysical research. Planets, 2017-07, Vol.122 (7), p.1458-1486

2017

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Thermal radiation of magma ocean planets using a 1‐D radiative‐convective model of H2O‐CO2 atmospheres

Journal of geophysical research. Planets, 2017-07, Vol.122 (7), p.1539-1553

2017

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Fat Plumes May Reflect the Complex Rheology of the Lower Mantle

Geophysical research letters, 2018-02, Vol.45 (3), p.1349-1354

2018

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Lithosphere Destabilization and Small‐Scale Convection Constrained From Geophysical Data and Analogical Models

Geochemistry, geophysics, geosystems : G3, 2021-03, Vol.22 (3), p.n/a

2021

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Global tomography using seismic hum

Geophysical journal international, 2016-02, Vol.204 (2), p.1222-1236

2016

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Characterization of Carbopol® hydrogel rheology for experimental tectonics and geodynamics

Tectonophysics, 2015-02, Vol.642, p.29-45

2015

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Early Formation of a Water Ocean as a Function of Initial CO2 and H2O Contents in a Solidifying Rocky Planet

Journal of geophysical research. Planets, 2023-08, Vol.128 (8), p.n/a

2023

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Accretion mode of oceanic ridges governed by axial mechanical strength

Nature geoscience, 2018-04, Vol.11 (4), p.274-279

2018

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Dynamical similarity and density (non-) proportionality in experimental tectonics

Tectonophysics, 2013-11, Vol.608, p.1371-1379

2013

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Dynamics of a laminar plume in a cavity: The influence of boundaries on the steady state stem structure

Geochemistry, geophysics, geosystems : G3, 2013-01, Vol.14 (1), p.158-178

2013

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Whole layer convection in a heterogeneous planetary mantle

Journal of Geophysical Research, 2004-03, Vol.109 (B3), p.B03403-n/a

2004

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Deflating the LLSVPs: Bundles of Mantle Thermochemical Plumes Rather Than Thick Stagnant “Piles”

Tectonics (Washington, D.C.), 2020-10, Vol.39 (10), p.n/a

2020

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Pacific geoid anomalies revisited in light of thermochemical oscillating domes in the lower mantle

Earth and planetary science letters, 2011-06, Vol.306 (1), p.123-135

2011

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The rheological behaviour of fracture-filling cherts: example of Barite Valley dikes, Barberton Greenstone Belt, South Africa

Solid earth (Göttingen), 2015-02, Vol.6 (1), p.253-269

2015

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Wavelet‐based directional analysis of the gravity field: evidence for large‐scale undulations

Geophysical journal international, 2012-06, Vol.189 (3), p.1430-1456

2012

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Heat flow and thickness of the lithosphere in the Canadian Shield

Journal of Geophysical Research, 1998-07, Vol.103 (B7), p.15269-15286

1998

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Onset of thermal convection in fluids with temperature-dependent viscosity: Application to the oceanic mantle

Journal of Geophysical Research - Solid Earth, 1994-10, Vol.99 (B10), p.19853-19866

1994

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Three distinct types of hotspots in the Earth’s mantle

Earth and planetary science letters, 2003-01, Vol.205 (3), p.295-308

2003

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Early Formation of a Water Ocean as a Function of Initial CO 2 and H 2 O Contents in a Solidifying Rocky Planet

Journal of geophysical research. Planets, 2023-08, Vol.128 (8)

2023

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Rheological control on the segmentation of the mid-ocean ridges: Laboratory experiments with extension initially perpendicular to the axis

Earth and planetary science letters, 2021-03, Vol.557, p.116706, Article 116706

2021

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Thermal evolution of an early magma ocean in interaction with the atmosphere: conditions for the condensation of a water ocean

BIO Web of Conferences, 2014-01, Vol.2, p.1006

2014

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Experimental and observational evidence for plume-induced subduction on Venus

The chemical composition of the Earth: Enstatite chondrite models

Formation and Evolution of Protoatmospheres

Thermal evolution of an early magma ocean in interaction with the atmosphere

The relative influence of H2O and CO2 on the primitive surface conditions and evolution of rocky planets

Thermal radiation of magma ocean planets using a 1‐D radiative‐convective model of H2O‐CO2 atmospheres

Fat Plumes May Reflect the Complex Rheology of the Lower Mantle

Lithosphere Destabilization and Small‐Scale Convection Constrained From Geophysical Data and Analogical Models

Global tomography using seismic hum

Characterization of Carbopol® hydrogel rheology for experimental tectonics and geodynamics

Early Formation of a Water Ocean as a Function of Initial CO2 and H2O Contents in a Solidifying Rocky Planet

Accretion mode of oceanic ridges governed by axial mechanical strength

Dynamical similarity and density (non-) proportionality in experimental tectonics

Dynamics of a laminar plume in a cavity: The influence of boundaries on the steady state stem structure

Whole layer convection in a heterogeneous planetary mantle

Deflating the LLSVPs: Bundles of Mantle Thermochemical Plumes Rather Than Thick Stagnant “Piles”

Pacific geoid anomalies revisited in light of thermochemical oscillating domes in the lower mantle

The rheological behaviour of fracture-filling cherts: example of Barite Valley dikes, Barberton Greenstone Belt, South Africa

Wavelet‐based directional analysis of the gravity field: evidence for large‐scale undulations

Heat flow and thickness of the lithosphere in the Canadian Shield

Onset of thermal convection in fluids with temperature-dependent viscosity: Application to the oceanic mantle

Three distinct types of hotspots in the Earth’s mantle

Early Formation of a Water Ocean as a Function of Initial CO 2 and H 2 O Contents in a Solidifying Rocky Planet

Rheological control on the segmentation of the mid-ocean ridges: Laboratory experiments with extension initially perpendicular to the axis

Thermal evolution of an early magma ocean in interaction with the atmosphere: conditions for the condensation of a water ocean

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