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Melting of peridotite to 140 gigapascals.

• Guillaume Fiquet, Anne Line Auzende, +4 authors Gastón Garbarino
• Science
• 2010

Interrogating physical processes that occur within the lowermost mantle is a key to understanding Earth's evolution and present-day inner composition. Among such processes, partial melting has been… (More)

Pressure-temperature estimates of the lizardite / antigorite transition in high pressure serpentinites

• Stéphane Schwartz, Stéphane Guillot, +5 authors Anne Line Auzende
• 2013

20 Serpentine minerals in natural samples are dominated by lizardite and antigorite. In 21 spite of numerous petrological experiments, the stability fields of these species remain poorly 22… (More)

Experimental investigation of As , Sb and Cs behavior during olivine serpentinization in hydrothermal alkaline systems

• Romain Lafay, German Montes-Hernandez, +5 authors Olivier Proux
• 2016

While Fluid-Mobile Elements (FMEs) such as B, Sb, Li, As or Cs are particularly concentrated in serpentinites, data on FME fluid–serpentine partitioning, distribution, and sequestration mechanisms… (More)

Experimental investigation of the stability of Fe-rich carbonates in the lower mantle

• Eglantine Boulard, Nicolas Menguy, +9 authors Guillaume Fiquet
• 2012

[1] The fate of carbonates in the Earth’s mantle plays a key role in the geodynamical carbon cycle. Although iron is a major component of the Earth’s lower mantle, the stability of Fe-bearing… (More)

Dissolution-reprecipitation and self-assembly of serpentine nanoparticles preceding chrysotile formation : Insights into the structure of proto-serpentine

• Romain Lafay, Anna Fernández, Martínez, Anne Line Auzende, Agnieszka Poulain
• 2016

Any poorly crystalline serpentine-type mineral with a lack of recognizable textural or diffraction features for typical serpentine varieties (i.e., chryotile, lizardite, and antigorite) is usually… (More)

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