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δ30Si and δ29Si determinations on USGS BHVO-1 and BHVO-2 reference materials with a new configuration on a nu plasma multi-collector ICP-MS
被引:98
作者:
Abraham, Kathrin
[1
,2
]
Opfergelt, Sophie
[2
,3
]
Fripiat, Francois
[2
,5
]
Cavagna, Anne-Julie
[2
,4
]
de Jong, Jeroen T. M.
[5
]
Foley, Stephen F.
[1
]
Andre, Luc
[2
]
Cardinal, Damien
[2
]
机构:
[1] Johannes Gutenberg Univ Mainz, Inst Geowissensch, D-55099 Mainz, Germany
[2] Musee Royal Afr Cent, Sect Mineral Petrog Geochim, B-3080 Tervuren, Belgium
[3] Univ Catholique Louvain, Unite Sci Sol, B-1348 Louvain, Belgium
[4] Vrije Univ Brussels, Dept Analyt & Environm Chem, B-1050 Brussels, Belgium
[5] Univ Libre Bruxelles, Dept Sci Terre & Environm, B-1050 Brussels, Belgium
关键词:
reference materials;
BHVO-1;
BHVO-2;
ocean island basalt;
silicon isotopes;
MC-ICP-MS;
D O I:
10.1111/j.1751-908X.2008.00879.x
中图分类号:
P3 [地球物理学];
P59 [地球化学];
学科分类号:
0708 ;
070902 ;
摘要:
We report silicon isotopic determinations for USGS rock reference materials BHVO-1 and BHVO-2 using a Nu Plasma multi-collector (MC)-ICP-MS, upgraded with a new adjustable entrance slit, to obtain medium resolution, as well as a stronger primary pump and newly designed sampler and skimmer cones ("B" cones). These settings, combined with the use of collector slits, allowed a resolution to be reached that was sufficient to overcome the (14)N(16)O and (14)N(2) interferences overlying the (30)Si and the (28)Si peaks, respectively, in an earlier set-up. This enabled accurate measurement of both delta(30)Si and delta(29)Si. The delta value is expressed in per mil variation relative to the NBS 28 quartz reference material. Based on data acquired from numerous sessions spread over a period of six months, we propose a recommended average delta(30)Si of -0.33 +/- 0.05 parts per thousand and -0.29 +/- 0.11 parts per thousand (2se) for BHVO-1 and BHVO-2, respectively. Our BHVO grand mean silicon isotope composition (delta(30)Si = -0.31 +/- 0.06 parts per thousand) is significantly more negative than the only published value for BHVO-2, but is in very good agreement with the recently established average value of ocean island basalts (OIB), confirming the conclusion that the OIB reservoir has a distinct isotopic composition from the solar reservoir as sampled by chondrites.
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页码:193 / 202
页数:10
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