High-precision trace element data for the USGS reference materials BCR-1, BCR-2, BHVO-1, BHVO-2, AGV-1, AGV-2, DTS-1, DTS-2, GSP-1 and GSP-2 by ID-TIMS and MIC-SSMS
I. Raczek et al., High-precision trace element data for the USGS reference materials BCR-1, BCR-2, BHVO-1, BHVO-2, AGV-1, AGV-2, DTS-1, DTS-2, GSP-1 and GSP-2 by ID-TIMS and MIC-SSMS, GEOSTAND N, 25(1), 2001, pp. 77-86
Citations number
13
Categorie Soggetti
Earth Sciences
Journal title
GEOSTANDARDS NEWSLETTER-THE JOURNAL OF GEOSTANDARDS AND GEOANALYSIS
Different batches of the new US Geological Survey (USGS) reference material
s (RMs) BCR-2, BHVO-2, AGV-2, DTS-2 and GSP-2 and the original USGS RMs BCR
-1, BHVO-1, AGV-1, DTS-1 and GSP-1 have been analysed by isotope dilution u
sing thermal ionisation mass spectrometry (ID-TIMS) and by multi-ion counti
ng spark source mass spectrometry (MIC-SSMS). The concentrations of K, Rb,
Sr, Ba and the rare earth elements were determined with overall analytical
uncertainties of better than 1% (ID-TIMS) and 3% (MIC-SSMS). The analyses o
f different aliquots; and batches of BCR-2, BHVO-2, AGV-2 and GSP-2, respec
tively, agree within 1%, i.e. approximately the analytical uncertainties of
the data. This indicates an homogeneous distribution of the trace elements
in these RMs. Differences in element concentrations of up to 17% in differ
ent aliquots; of the depleted RM DTS-2 are outside the analytical uncertain
ty of our data. They may be attributed to a slightly heterogeneous distribu
tion of trace elements in this dunite sample. Our trace element data for BC
R-2, BHVO-2, AGV-2 and GSP-2 agree within about 3% with preliminary referen
ce values published by the USGS. They also agree within 1-6% with those of
the original RMs BCR-1, BHVO-1, AGV-1 and GSP-1. Large compositional differ
ences are found between DTS-2 and DTS-1, where the concentrations of K. Rb,
Sr and the light REE differ by factors of 2 to 24.