6533b86efe1ef96bd12cc0af

RESEARCH PRODUCT

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

Sophie OpfergeltKathrin AbrahamStephen F. FoleyDamien CardinalFrançois FripiatLuc AndréJeroen De JongA. J. Cavagna

subject

DeltaAnalytical chemistryMineralogyGeologyPlasmaOcean island basaltMedium resolutionGeochemistry and PetrologyChondriteIsotopes of siliconMC-ICP-MSQuartzInductively coupled plasma mass spectrometryGeology

description

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 (NO)-N-14-O-16 and N-14(2) interferences overlying the Si-30 and the Si-28 peaks, respectively, in an earlier set-up. This enabled accurate measurement of both delta Si-30 and delta Si-29. 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 Si-30 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 Si-30 = -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.

10.1111/j.1751-908x.2008.00879.xhttps://hdl.handle.net/20.500.14017/6cae407c-b9fd-4408-b855-e022fe7d6a39