PRELIMINARY UVLAMP DETERMINATIONS OF ARGON PARTITION COEFFICIENTS FOR OLIVINE AND CLINOPYROXENE GROWN FROM SILICATE MELTS

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dc.contributor.author Brooker R.A.
dc.contributor.author Carroll M.R.
dc.contributor.author Draper D.S.
dc.contributor.author Wartho J.A.
dc.contributor.author Kelley S.P.
dc.date.accessioned 2021-01-06T07:51:19Z
dc.date.available 2021-01-06T07:51:19Z
dc.date.issued 1998
dc.identifier https://elibrary.ru/item.asp?id=31855177
dc.identifier.citation Chemical Geology, 1998, , 1, 185-200
dc.identifier.issn 0009-2541
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/22298
dc.description.abstract An ultra-violet laser ablation microprobe (UVLAMP) has been applied for the first time to investigate argon partition coefficients for olivines and clinopyroxenes grown from silicate melts at 1 bar argon pressure. These preliminary measurements yield crystal/melt partition coefficients ranging from 0.138 (±0.01) to 0.013 (±0.003) for olivine and 0.589 (±0.003) to 0.0016 (±0.0005) for clinopyroxene. The higher values may indicate sub-microscopic melt inclusions, or some other heterogeneous distributions of `non-equilibrium' argon in the crystals. The lower values are probably more representative of true partition coefficients and fall at least an order of magnitude below the previously reported experimental data. The possibility of anomalous, high argon contents for crystals in previous studies is discussed in terms of surface adsorption, `trapped' argon and early partial melting.
dc.title PRELIMINARY UVLAMP DETERMINATIONS OF ARGON PARTITION COEFFICIENTS FOR OLIVINE AND CLINOPYROXENE GROWN FROM SILICATE MELTS
dc.type Статья


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