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Alexandre Corgne

Researcher at Austral University of Chile

Publications -  43
Citations -  2715

Alexandre Corgne is an academic researcher from Austral University of Chile. The author has contributed to research in topics: Silicate & Mantle (geology). The author has an hindex of 24, co-authored 41 publications receiving 2331 citations. Previous affiliations of Alexandre Corgne include University of Toulouse & Carnegie Institution for Science.

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Melting of Peridotite to 140 Gigapascals

TL;DR: Melting phase relations and element partitioning data show that these liquids could host many incompatible elements at the base of the mantle, such that seismically anomalous zones near the boundary between the core and the mantle may result from isolated pockets of melt.
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An experimental study of element partitioning between magnetite, clinopyroxene and iron-bearing silicate liquids with particular emphasis on vanadium

TL;DR: In this paper, vanadium partitioning is strongly dependent on oxygen fugacity, decreasing by approximately one order of magnitude with increasing oxygen fugancy, from 0.7 to 2.6 log units above the NNO buffer.
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Systematics of metal-silicate partitioning for many siderophile elements applied to Earth’s core formation

TL;DR: In this article, the effects of temperature, oxygen fugacity and silicate melt composition on superliquidus metal-silicate partitioning were investigated for a number of moderately siderophile (Mo, As, Ge, W, V, P, Ni, Co, Cr, Zn, Mn and W) and refractory lithophile (Nb, Ta) elements.
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Silicate perovskite-melt partitioning of trace elements and geochemical signature of a deep perovskitic reservoir

TL;DR: In this article, the authors determined the partitioning of a wide range of trace elements between silicate melts and MgSiO3 perovskites using both laser ablation-ICPMS and ion microprobe techniques.
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Spin transition and equations of state of (Mg, Fe)O solid solutions

TL;DR: In this article, a series of experiments were performed to investigate the compositional effect on the compression behavior of (Mg, Fe)O solid solutions at high pressure and found abnormal volume contractions at about 40, 60, and 80 GPa.