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Denis Andrault

PROF UNIV

Université Clermont Auvergne

France

Research Interests

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About

Denis Andrault is a Professor at Université Clermont Auvergne in France. His research areas include petrology, geophysics, and the thermochemical state of the Earth's interior, as evidenced by recent articles focusing on topics such as low melt viscosity in Earth’s mantle, the seismic structure of the Martian mantle, and conditions for segregation within magma oceans. He is dedicated to advancing the understanding of planetary sciences through experimental and theoretical approaches.

Articles (17)

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2026

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2025

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2025

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2025

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2025

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2025

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2024

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2023

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2022

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2022

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2022

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2021

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2020

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2020

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2020

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2020

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2020

Collaborators (8)

Yingwei Fei

Staff

Carnegie Institution for Science

UNITED STATES

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Oliver Lord

Senior Lecturer & Head of Petrology

University of Bristol

UNITED KINGDOM

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Takashi Yoshino

Professor

JAPAN

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Tatsuhiko Kawamoto

Professor

Shizuoka University

JAPAN

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Bin Zhao

JAPAN

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Noriyoshi Tsujino

Japan Synchrotron Radiation Research Institute

JAPAN

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Guillaume Morard

CNRS Researcher

FRANCE

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David Dobson

University College London

UNITED KINGDOM

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Denis Andrault

Research Interests

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Articles (17)

Aluminium drives hydrogen incorporation in pyrolitic lower mantle: Constraints from a combined FTIR-ERDA-nanoSIMS analysis

Low melt viscosity enables melt doublets above the 410-km discontinuity

Low melt viscosity enables melt doublets above the 410-km discontinuity

Equilibrium melting relations at shallow lower mantle P-T conditions probed by the laser-heated diamond anvil cell

Long-lived magnetic field in earth-like terrestrial planets

Seismic structure of Martian mantle inferred from in situ sound velocity measurements

The high flux nano-X-ray diffraction, fluorescence and imaging beamline ID27 for science under extreme conditions on the ESRF Extremely Brilliant Source

Conditions for Segregation of a Crystal‐Rich Layer Within a Convective Magma Ocean

Deep mantle origin of large igneous provinces and komatiites

Solidus melting of pyrolite and bridgmanite: Implication for the thermochemical state of the Earth's interior

Comment on: Melting behavior of SiO2 up to 120 GPa (Andrault et al. 2020)

Direct Viscosity Measurement of Peridotite Melt to Lower‐Mantle Conditions: A Further Support for a Fractional Magma‐Ocean Solidification at the Top of the Lower Mantle

Melting behavior of SiO2 up to 120 GPa

Melting behavior of SiO2 up to 120 GPa

Formation of bridgmanite-enriched layer at the top lower-mantle during magma ocean solidification

Formation of bridgmanite-enriched layer at the top lower-mantle during magma ocean solidification

A mushy Earth's mantle for more than 500 Myr after the magma ocean solidification

Collaborators (8)

Yingwei Fei

Oliver Lord

Takashi Yoshino

Tatsuhiko Kawamoto

Bin Zhao

Noriyoshi Tsujino

Guillaume Morard

David Dobson

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