SUBSOLIDUS REE PARTITIONING BETWEEN PYROXENE AND PLAGIOCLASE IN CUMULATE EUCRITES: AN ION MICROPROBE INVESTIGATION
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dc.contributor.author | Pun A. | |
dc.contributor.author | Papike J.J. | |
dc.contributor.author | Layne G.D. | |
dc.date.accessioned | 2020-12-17T04:15:20Z | |
dc.date.available | 2020-12-17T04:15:20Z | |
dc.date.issued | 1997 | |
dc.identifier | https://elibrary.ru/item.asp?id=275067 | |
dc.identifier.citation | Geochimica et Cosmochimica Acta, 1997, , 23, 5089-5097 | |
dc.identifier.issn | 0016-7037 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/20988 | |
dc.description.abstract | In an attempt to elucidate the relationship between the cumulate eucrites and the noncumulate (main series) eucrites, we have examined the trace-element systematics of plagioclase grains that coexist with inverted pigeonites of the cumulate eucrites. Analyses were done by secondary ion mass spectrometry (SIMS). Plagioclase compositions are uniform in trace-element abundances within grains from each cumulate eucrite, but are variable between the four analyzed: Moama, Moore County, Serra de Mage, and Binda. Shapes of CI-normalized trace-element abundance patterns of the plagioclase grains of the cumulates are typical of plagioclase, showing a LREE-enriched pattern with positive Eu anomalies reflecting the site preference of Eu2+ in the feldspar structure.Using trace-element concentrations of the pyroxenes (orthopyroxene, pigeonite, augite; Pun and Papike, 1995) and plagioclase (this study), we calculate the subsolidus partition coefficients (Ds) for the REEs and Y between plagioclase and pyroxenes in the examined cumulate eucrites. Trace-element systematics suggest that igneous trace-element signatures have been altered by subsolidus exchange for both the plagioclase and pyroxene. Calculated hypothetical parental-melt patterns determined from pyroxene and plagioclase are different and can differ by a factor of 4-5 for individual REEs. | |
dc.title | SUBSOLIDUS REE PARTITIONING BETWEEN PYROXENE AND PLAGIOCLASE IN CUMULATE EUCRITES: AN ION MICROPROBE INVESTIGATION | |
dc.type | Статья |
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