Particular H 2 O dissolution mechanism in iron‐rich melt: Application to martian basaltic melt genesis

The high melting temperature of pure iron under core-mantle boundary (4250 ± 250 K), here determined by X-ray absorption experiments at the Fe K-edge, indicates that volatile

Induced magnetic anisotropy is likely to arise from the redis- tribution of atoms between the different sites and the relative abundance of such sites as well as the chemical

Fe(III)-bearing basaltic glasses (MORB2, MORB3) and Fe-free glass (HAPLO) in the presence of 119.. siderophores and then in the presence of the

The experiment with 17.5 vol% Fe-S in the olivine aggregate maintains a stable high electrical conductivity over 94 h at temperatures above the Fe-S melting

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des

GALAS, "Local structures about some transition elements in oxide glasses using X-ray absorption spectroscopy", Journal de Physique, Tome 43, pp. BUFFAT, "Influence

1) Because Fe S+ needs the neighbourhood of alkali ions for charge compensation for its different coordJnations, these alkali metals directly participate in the structure of the

As already remarked, many of the iron lines in the infra-red are susceptible to pressure broadening and have line profiles with a significant Lorentzian component; this is