EXPERIMENTAL DETERMINATION OF THE PARTITIONING BEHAVIOR OF RARE EARTH AND HIGH FIELD STRENGTH ELEMENTS BETWEEN PARGASITIC AMPHIBOLE AND NATURAL SILICATE MELTS

dc.contributor.author	Hilyard M.
dc.contributor.author	Nielsen R.L.
dc.contributor.author	Beard J.S.
dc.contributor.author	Patinõ-Douce A.
dc.contributor.author	Blencoe J.
dc.date.accessioned	2021-01-29T07:11:10Z
dc.date.available	2021-01-29T07:11:10Z
dc.date.issued	2000
dc.identifier	https://elibrary.ru/item.asp?id=13792541
dc.identifier.citation	Geochimica et Cosmochimica Acta, 2000, 64, 6, 1103-1120
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/24013
dc.description.abstract	The primary goal of this investigation was to derive a set of expressions that can be used to calculate the amphibole-melt partitioning behavior of the rare earth elements (REE) and the high field strength elements (HFSE) in natural systems. To supplement the existing data set on basaltic systems, we conducted experiments on systems where amphibole was in equilibrium with dacitic, tonalitic and low Si rhyolitic melts. These experiments, doped with La, Sm, Gd, Lu, Ta, Nb, Y, Zr, and Hf, were run at pressures of 2 and 5 kbar, temperatures between 900°C and 945°C, and oxidation conditions ranging from QFM-1 to NiNiO+1.
dc.title	EXPERIMENTAL DETERMINATION OF THE PARTITIONING BEHAVIOR OF RARE EARTH AND HIGH FIELD STRENGTH ELEMENTS BETWEEN PARGASITIC AMPHIBOLE AND NATURAL SILICATE MELTS
dc.type	Статья

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