Frederic Moynier

France

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Articles (21)

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2025

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2020

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2020

Collaborators (11)

Julien Siebert

Université Paris-Saclay

FRANCE

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Razvan Caracas

University of Oslo

NORWAY

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Baptiste Debret

Institut de Physique du Globe de Paris

FRANCE

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Ke ZHU

University of Bristol

UNITED KINGDOM

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Angela Limare

Institut de Physique du Globe de Paris

FRANCE

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Fred Jourdan

Professor / Director of the Western Australia Argon Isotope Facility

Curtin University

AUSTRALIA

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Paolo Angelo Sossi

Assistant Professor

ETH Zürich

SWITZERLAND

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James Day

Professor

Scripps Institution of Oceanography

UNITED STATES

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Sebastian Tappe

Professor

University of Tromsø - The Arctic University of Norway

NORWAY

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Zhengrong Wang

Associate Professor

The City College of New York

UNITED STATES

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Troels Haugbølle

Københavns Universitet

DENMARK

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Frederic Moynier

Research Interests

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Articles (21)

Impact-induced sublimation drives volatile depletion in carbonaceous meteorites

Heavy potassium isotopes in carbonatites reveal oceanic crust subduction as the driver of deep carbon cycling

Carbonate metasomatism at mantle wedge conditions, evidence from trace element and stable isotope (Fe, Zn) signatures of orogenic peridotites

Copper isotope evidence for recycled crustal sulfides in deep mantle plume source

Degasing of Phobos in a giant impact scenario: Implications for the MMX sample return mission

A whole-scale volatile-depleted lunar interior

Chemical compositions of Chang’e-6 lunar soil and substantial addition of noritic crust ejecta from Apollo basin

Determination of K Isotope Compositions in Sedimentary Rocks and Their Implications for Discriminating Sediment Origin

Earth’s K recycling: Perspective from K isotopes of intracontinental magmas

Hydrodynamical simulations of proto-Moon degassing

Nickel and Chromium Stable Isotopic Composition of Ureilites: Implications for the Earth's Core Formation and Differentiation of the Ureilite Parent Body

Hybrid Accretion of Carbonaceous Chondrites by Radial Transport across the Jupiter Barrier

Chromium isotopic insights into the origin of chondrite parent bodies and the early terrestrial volatile depletion

A condensation origin for the mass-dependent silicon isotopic variations in Allende components: implications for complementarity

Citation for the 2020 EAG Houtermans Award to Kun Wang

Conditions and extent of volatile loss from the Moon during formation of the Procellarum basin

Potassium isotopic composition of various samples using a dual-path collision cell-capable multiple-collector inductively coupled plasma mass spectrometer, Nu instruments Sapphire

Simultaneous determination of mass-dependent Mg isotopic variations and radiogenic <sup>26</sup>Mg by laser ablation-MC-ICP-MS and implications for the formation of chondrules

Study on the Isotope fractionation of Zinc in Complexation with Macrocyclic Polyethers

An experimentally-determined general formalism for evaporation and isotope fractionation of Cu and Zn from silicate melts between 1300 and 1500 °C and 1 bar

Mass-independent and mass-dependent Cr isotopic composition of the Rumuruti (R) chondrites: Implication for their origin and their significance for planet formation

Collaborators (11)

Julien Siebert

Razvan Caracas

Baptiste Debret

Ke ZHU

Angela Limare

Fred Jourdan

Paolo Angelo Sossi

James Day

Sebastian Tappe

Zhengrong Wang

Troels Haugbølle

Make your next move.

Frederic Moynier

Research Interests

Explore related searches

Contact this professor

Articles (21)

Impact-induced sublimation drives volatile depletion in carbonaceous meteorites

Heavy potassium isotopes in carbonatites reveal oceanic crust subduction as the driver of deep carbon cycling

Carbonate metasomatism at mantle wedge conditions, evidence from trace element and stable isotope (Fe, Zn) signatures of orogenic peridotites

Copper isotope evidence for recycled crustal sulfides in deep mantle plume source

Degasing of Phobos in a giant impact scenario: Implications for the MMX sample return mission

A whole-scale volatile-depleted lunar interior

Chemical compositions of Chang’e-6 lunar soil and substantial addition of noritic crust ejecta from Apollo basin

Determination of K Isotope Compositions in Sedimentary Rocks and Their Implications for Discriminating Sediment Origin

Earth’s K recycling: Perspective from K isotopes of intracontinental magmas

Hydrodynamical simulations of proto-Moon degassing

Nickel and Chromium Stable Isotopic Composition of Ureilites: Implications for the Earth's Core Formation and Differentiation of the Ureilite Parent Body

Hybrid Accretion of Carbonaceous Chondrites by Radial Transport across the Jupiter Barrier

Chromium isotopic insights into the origin of chondrite parent bodies and the early terrestrial volatile depletion

A condensation origin for the mass-dependent silicon isotopic variations in Allende components: implications for complementarity

Citation for the 2020 EAG Houtermans Award to Kun Wang

Conditions and extent of volatile loss from the Moon during formation of the Procellarum basin

Potassium isotopic composition of various samples using a dual-path collision cell-capable multiple-collector inductively coupled plasma mass spectrometer, Nu instruments Sapphire

Simultaneous determination of mass-dependent Mg isotopic variations and radiogenic <sup>26</sup>Mg by laser ablation-MC-ICP-MS and implications for the formation of chondrules

Study on the Isotope fractionation of Zinc in Complexation with Macrocyclic Polyethers

An experimentally-determined general formalism for evaporation and isotope fractionation of Cu and Zn from silicate melts between 1300 and 1500 °C and 1 bar

Mass-independent and mass-dependent Cr isotopic composition of the Rumuruti (R) chondrites: Implication for their origin and their significance for planet formation

Collaborators (11)

Julien Siebert

Razvan Caracas

Baptiste Debret

Ke ZHU

Angela Limare

Fred Jourdan

Paolo Angelo Sossi

James Day

Sebastian Tappe

Zhengrong Wang

Troels Haugbølle

Make your next move.

An experimentally-determined general formalism for evaporation and isotope fractionation of Cu and Zn from silicate melts between 1300 and 1500 °C and 1 bar