DOIAbstract
International audienceA study of cerium in zircon minerals has allowed an assessment of the redox conditions that prevailed when Earth's earliest magmas formed. The results suggest that the mantle became oxidized sooner than had been though
International audienceA study of cerium in zircon minerals has allowed an assessment of the redox conditions that prevailed when Earth's earliest magmas formed. The results suggest that the mantle became oxidized sooner than had been though
Chemical reduction-oxidation mechanisms within mantle rocks link to the terrestrial carbon cycle by ...
International audienceThe basic aspects of redox geochemistry are reviewed to provide a useful compe...
Earth surface redox conditions are intimately linked to the co-evolution of the geosphere and biosph...
International audienceA study of cerium in zircon minerals has allowed an assessment of the redox co...
Geochemical and petrologic tools were deployed to investigate the redox state and water content of t...
In order to determine the evolution of the redox state of the mantle, the oxygen fugacities of sixte...
The distribution of volatile elements between Earth's core, mantle, and atmosphere over the last 4.5...
International audienceThe Earth's mantle redox state regulates the fate and transfer of metals by ma...
International audienceIt is widely believed that the Earth was strongly reduced during its early acc...
Redox melting refers to any process by which melt is generated by the contact of a rock with a fluid...
Exchange between a magma ocean and vapor produced Earth's earliest atmosphere. Its speciation depend...
The oxidation state of the Earth's mantle during formation remains an unresolved question, whether i...
AbstractUsing a newly-calibrated relation for cerium redox equilibria in silicate melts (Smythe and ...
We present an analytical method to quantify the absolute redox capacity, ΔO2, of geological material...
Magma oceans (MOs) are episodes of large-scale melting of the mantle of terrestrial planets. The ene...
Chemical reduction-oxidation mechanisms within mantle rocks link to the terrestrial carbon cycle by ...
International audienceThe basic aspects of redox geochemistry are reviewed to provide a useful compe...
Earth surface redox conditions are intimately linked to the co-evolution of the geosphere and biosph...
International audienceA study of cerium in zircon minerals has allowed an assessment of the redox co...
Geochemical and petrologic tools were deployed to investigate the redox state and water content of t...
In order to determine the evolution of the redox state of the mantle, the oxygen fugacities of sixte...
The distribution of volatile elements between Earth's core, mantle, and atmosphere over the last 4.5...
International audienceThe Earth's mantle redox state regulates the fate and transfer of metals by ma...
International audienceIt is widely believed that the Earth was strongly reduced during its early acc...
Redox melting refers to any process by which melt is generated by the contact of a rock with a fluid...
Exchange between a magma ocean and vapor produced Earth's earliest atmosphere. Its speciation depend...
The oxidation state of the Earth's mantle during formation remains an unresolved question, whether i...
AbstractUsing a newly-calibrated relation for cerium redox equilibria in silicate melts (Smythe and ...
We present an analytical method to quantify the absolute redox capacity, ΔO2, of geological material...
Magma oceans (MOs) are episodes of large-scale melting of the mantle of terrestrial planets. The ene...
Chemical reduction-oxidation mechanisms within mantle rocks link to the terrestrial carbon cycle by ...
International audienceThe basic aspects of redox geochemistry are reviewed to provide a useful compe...
Earth surface redox conditions are intimately linked to the co-evolution of the geosphere and biosph...
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