Silicate diffusion in alkali-carbonatite and hydrous melts at 16.5 and 24GPa: Implication for the melt transport by dissolution-precipitation in the transition zone and uppermost lower mantle

Physics of the Earth and Planetary Interiors

Volumn 225, Issue , 2013, Pages 1-11

  Shatskiy, Anton ^a,b   Litasov, Konstantin D ^a,b   Borzdov, Yuriy M ^a   Katsura, Tomoo ^c   Yamazaki, Daisuke ^d   Ohtani, Eiji ^e  

^a SOBOLEV INSTITUTE OF GEOLOGY AND MINERALOGY   (Russian Federation)

^b NOVOSIBIRSK STATE UNIVERSITY   (Russian Federation)

^c UNIVERSITÄT BAYREUTH   (Germany)

^d OKAYAMA UNIVERSITY   (Japan)

^e TOHOKU UNIVERSITY   (Japan)

Author keywords

Carbonatite; Diffusion; Dissolution precipitation; Earth's mantle; Hydrous melt; Kimberlite; Melt percolation

Indexed keywords

CARBONATITES; DISSOLUTION PRECIPITATIONS; EARTH'S MANTLE; HYDROUS MELTS; KIMBERLITE; MELT PERCOLATIONS;

DIFFUSION; DISSOLUTION; DROPS; EXPERIMENTS; MINERALS; SILICATES; SOLVENTS; THERMAL GRADIENTS; THERMAL PLUMES; VOLCANIC ROCKS;

SEGREGATION (METALLOGRAPHY);

CARBONATITE; DIFFUSION; DISSOLUTION; EXPERIMENTAL MINERALOGY; EXPERIMENTAL STUDY; KIMBERLITE; LOWER MANTLE; MANTLE STRUCTURE; MELT INCLUSION; PERCOLATION; PRECIPITATION (CHEMISTRY); PRESSURE EFFECT; SILICATE; SILICATE MINERAL; WADSLEYITE;

EID: 84888298973     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2013.09.004     Document Type: Article

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