TRACE ELEMENT PARTITIONING BETWEEN PLAGIOCLASE AND MELT: INVESTIGATION OF DOPANT INFLUENCE ON PARTITION BEHAVIOR

dc.contributor.authorBindeman I.N.
dc.contributor.authorDavis A.M.
dc.date.accessioned2021-01-30T12:21:12Z
dc.date.available2021-01-30T12:21:12Z
dc.date.issued2000
dc.description.abstractWe present results from an ion microprobe study of REE-doped and natural concentration plagioclase-basalt run products of Drake (1972) that carries on from our earlier study (Bindeman et al., 1998). The goals of this work are (1) to determine plagioclase/melt partition coefficients for all REE for four analyzed plagioclase compositions (An40–80); and (2) to determine whether doping with REE influences partition coefficients of other REE and other trace elements. In combination with our analyses of Sr-doped runs (Bindeman et al., 1998), the new data allow us to compare partition coefficients (Dι’s) of trace elements at natural concentrations with those in REE-doped and Sr-doped runs. In these comparisons, runs have the same run temperature and compositions, but different doping element(s).
dc.identifierhttps://elibrary.ru/item.asp?id=13895028
dc.identifier.citationGeochimica et Cosmochimica Acta, 2000, 64, 16, 2863-2878
dc.identifier.issn0016-7037
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/24045
dc.titleTRACE ELEMENT PARTITIONING BETWEEN PLAGIOCLASE AND MELT: INVESTIGATION OF DOPANT INFLUENCE ON PARTITION BEHAVIOR
dc.typeСтатья

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