MINERAL-AQUEOUS FLUID PARTITIONING OF TRACE ELEMENTS AT 900-1200°C AND 3.0-5.7 GPA: NEW EXPERIMENTAL DATA FOR GARNET, CLINOPYROXENE, AND RUTILE, AND IMPLICATIONS FOR MANTLE METASOMATISM

dc.contributor.author	Stalder R.
dc.contributor.author	Foley S.F.
dc.contributor.author	Drey G.P.
dc.contributor.author	Horn I.
dc.date.accessioned	2021-01-04T07:57:21Z
dc.date.available	2021-01-04T07:57:21Z
dc.date.issued	1998
dc.identifier	https://elibrary.ru/item.asp?id=31127458
dc.identifier.citation	Geochimica et Cosmochimica Acta, 1998, , 10, 1781-1801
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22206
dc.description.abstract	In order to constrain the role of fluid phases during metasomatic processes in the upper mantle, trace element partition coefficients for Ba, Sr, Pb, Nb, Ta, Zr, Hf, Ti, La, Ce, Sm, Tb, and Yb between aqueous fluids and eclogite assemblage minerals (garnet, clinopyroxene, and rutile) have been determined experimentally at 900–1200°C and 3.0–5.7 GPa. Using a new experimental technique in which diamond aggregates are added to the experimental capsule set-up, the fluid was separated from the solid residue so that both quenched solute and residual minerals could be analysed directly. Trace element concentrations were determined in situ by laser ablation microprobe (LAM).
dc.title	MINERAL-AQUEOUS FLUID PARTITIONING OF TRACE ELEMENTS AT 900-1200°C AND 3.0-5.7 GPA: NEW EXPERIMENTAL DATA FOR GARNET, CLINOPYROXENE, AND RUTILE, AND IMPLICATIONS FOR MANTLE METASOMATISM
dc.type	Статья

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