Isotope dilution MC-ICP-MS rare earth element analysis of geochemical reference materials NIST SRM 610, NIST SRM 612, NIST SRM 614, BHVO-2G, BHVO-2, BCR-2G, JB-2, WS-E, W-2, AGV-1 and AGV-2

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Isotope dilution MC-ICP-MS rare earth element analysis of geochemical reference materials NIST SRM 610, NIST SRM 612, NIST SRM 614, BHVO-2G, BHVO-2, BCR-2G, JB-2, WS-E, W-2, AGV-1 and AGV-2. / Kent, Adam J.R.; Jacobsen, Benjamin; Peate, David W.; Waight, Tod E.; Baker, Joel A.

I: Geostandards and Geoanalytical Research, Bind 28, Nr. 3, 01.01.2004, s. 417-429.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Kent, AJR, Jacobsen, B, Peate, DW, Waight, TE & Baker, JA 2004, 'Isotope dilution MC-ICP-MS rare earth element analysis of geochemical reference materials NIST SRM 610, NIST SRM 612, NIST SRM 614, BHVO-2G, BHVO-2, BCR-2G, JB-2, WS-E, W-2, AGV-1 and AGV-2', Geostandards and Geoanalytical Research, bind 28, nr. 3, s. 417-429. https://doi.org/10.1111/j.1751-908X.2004.tb00760.x

APA

Kent, A. J. R., Jacobsen, B., Peate, D. W., Waight, T. E., & Baker, J. A. (2004). Isotope dilution MC-ICP-MS rare earth element analysis of geochemical reference materials NIST SRM 610, NIST SRM 612, NIST SRM 614, BHVO-2G, BHVO-2, BCR-2G, JB-2, WS-E, W-2, AGV-1 and AGV-2. Geostandards and Geoanalytical Research, 28(3), 417-429. https://doi.org/10.1111/j.1751-908X.2004.tb00760.x

Vancouver

Kent AJR, Jacobsen B, Peate DW, Waight TE, Baker JA. Isotope dilution MC-ICP-MS rare earth element analysis of geochemical reference materials NIST SRM 610, NIST SRM 612, NIST SRM 614, BHVO-2G, BHVO-2, BCR-2G, JB-2, WS-E, W-2, AGV-1 and AGV-2. Geostandards and Geoanalytical Research. 2004 jan. 1;28(3):417-429. https://doi.org/10.1111/j.1751-908X.2004.tb00760.x

Author

Kent, Adam J.R. ; Jacobsen, Benjamin ; Peate, David W. ; Waight, Tod E. ; Baker, Joel A. / Isotope dilution MC-ICP-MS rare earth element analysis of geochemical reference materials NIST SRM 610, NIST SRM 612, NIST SRM 614, BHVO-2G, BHVO-2, BCR-2G, JB-2, WS-E, W-2, AGV-1 and AGV-2. I: Geostandards and Geoanalytical Research. 2004 ; Bind 28, Nr. 3. s. 417-429.

Bibtex

@article{fd6c30e64b3a41ad90b967020427d3fd,
title = "Isotope dilution MC-ICP-MS rare earth element analysis of geochemical reference materials NIST SRM 610, NIST SRM 612, NIST SRM 614, BHVO-2G, BHVO-2, BCR-2G, JB-2, WS-E, W-2, AGV-1 and AGV-2",
abstract = "We present data for the concentrations of eleven rare earth elements (La, Ce, Pr, Nd, Sm, Eu, Gd, Dy, Er, Yb, Lu) in eleven international geochemical reference materials obtained by isotope dilution multi-collector inductively coupled plasma-mass spectrometry (MC-ICP-MS). We have analysed both rock powders and synthetic silicate glasses, and the latter provide precise data to support the use of these as reference materials for in situ trace element determination techniques. Our data also provide precise measurements of the abundance of mono-isotopic Pr in both glasses and powders, which allows more accurate constraints on the anomalous redox-related behaviour of Ce during geochemical processes. All materials were analysed in replicate providing data that typically reproduce to better than one percent. Sm/Nd ratios in all these materials also reproduce to better than 0.2% and are accurate to < 0.2% and can thus be used as calibrants for Sm-Nd geochronology. Our analyses agree well with existing data on these reference materials. In particular, for NIST SRM 610, USGS BHVO-2, AGV-1 and AGV-2, our measured REE abundances are typically within 2% (and mostly 1%) of REE concentrations previously determined by isotope dilution analysis and thermal ionisation mass spectrometry, consistent with the higher degree of precision and accuracy obtained from isotope dilution techniques. Close agreement of results between basaltic glass reference materials USGS BHVO-2G and BCR-2G and the BHVO-2 and BCR-2 powders from which they were created suggests that little fractionation, concentration or dilution of REE contents occurred during glass manufacture.",
keywords = "AGV-1, AGV-2, BCR-2G, BHVO-2, BVHO-2G, Isotope dilution, JB-2, MC-ICP-MS, NIST SRM 610, NIST SRM 612, NIST SRM 614, Rare earth elements, Reference materials, W-2, WS-E",
author = "Kent, {Adam J.R.} and Benjamin Jacobsen and Peate, {David W.} and Waight, {Tod E.} and Baker, {Joel A.}",
year = "2004",
month = jan,
day = "1",
doi = "10.1111/j.1751-908X.2004.tb00760.x",
language = "English",
volume = "28",
pages = "417--429",
journal = "Geostandards and Geoanalytical Research",
issn = "1639-4488",
publisher = "Wiley-Blackwell",
number = "3",

}

RIS

TY - JOUR

T1 - Isotope dilution MC-ICP-MS rare earth element analysis of geochemical reference materials NIST SRM 610, NIST SRM 612, NIST SRM 614, BHVO-2G, BHVO-2, BCR-2G, JB-2, WS-E, W-2, AGV-1 and AGV-2

AU - Kent, Adam J.R.

AU - Jacobsen, Benjamin

AU - Peate, David W.

AU - Waight, Tod E.

AU - Baker, Joel A.

PY - 2004/1/1

Y1 - 2004/1/1

N2 - We present data for the concentrations of eleven rare earth elements (La, Ce, Pr, Nd, Sm, Eu, Gd, Dy, Er, Yb, Lu) in eleven international geochemical reference materials obtained by isotope dilution multi-collector inductively coupled plasma-mass spectrometry (MC-ICP-MS). We have analysed both rock powders and synthetic silicate glasses, and the latter provide precise data to support the use of these as reference materials for in situ trace element determination techniques. Our data also provide precise measurements of the abundance of mono-isotopic Pr in both glasses and powders, which allows more accurate constraints on the anomalous redox-related behaviour of Ce during geochemical processes. All materials were analysed in replicate providing data that typically reproduce to better than one percent. Sm/Nd ratios in all these materials also reproduce to better than 0.2% and are accurate to < 0.2% and can thus be used as calibrants for Sm-Nd geochronology. Our analyses agree well with existing data on these reference materials. In particular, for NIST SRM 610, USGS BHVO-2, AGV-1 and AGV-2, our measured REE abundances are typically within 2% (and mostly 1%) of REE concentrations previously determined by isotope dilution analysis and thermal ionisation mass spectrometry, consistent with the higher degree of precision and accuracy obtained from isotope dilution techniques. Close agreement of results between basaltic glass reference materials USGS BHVO-2G and BCR-2G and the BHVO-2 and BCR-2 powders from which they were created suggests that little fractionation, concentration or dilution of REE contents occurred during glass manufacture.

AB - We present data for the concentrations of eleven rare earth elements (La, Ce, Pr, Nd, Sm, Eu, Gd, Dy, Er, Yb, Lu) in eleven international geochemical reference materials obtained by isotope dilution multi-collector inductively coupled plasma-mass spectrometry (MC-ICP-MS). We have analysed both rock powders and synthetic silicate glasses, and the latter provide precise data to support the use of these as reference materials for in situ trace element determination techniques. Our data also provide precise measurements of the abundance of mono-isotopic Pr in both glasses and powders, which allows more accurate constraints on the anomalous redox-related behaviour of Ce during geochemical processes. All materials were analysed in replicate providing data that typically reproduce to better than one percent. Sm/Nd ratios in all these materials also reproduce to better than 0.2% and are accurate to < 0.2% and can thus be used as calibrants for Sm-Nd geochronology. Our analyses agree well with existing data on these reference materials. In particular, for NIST SRM 610, USGS BHVO-2, AGV-1 and AGV-2, our measured REE abundances are typically within 2% (and mostly 1%) of REE concentrations previously determined by isotope dilution analysis and thermal ionisation mass spectrometry, consistent with the higher degree of precision and accuracy obtained from isotope dilution techniques. Close agreement of results between basaltic glass reference materials USGS BHVO-2G and BCR-2G and the BHVO-2 and BCR-2 powders from which they were created suggests that little fractionation, concentration or dilution of REE contents occurred during glass manufacture.

KW - AGV-1

KW - AGV-2

KW - BCR-2G

KW - BHVO-2

KW - BVHO-2G

KW - Isotope dilution

KW - JB-2

KW - MC-ICP-MS

KW - NIST SRM 610

KW - NIST SRM 612

KW - NIST SRM 614

KW - Rare earth elements

KW - Reference materials

KW - W-2

KW - WS-E

UR - http://www.scopus.com/inward/record.url?scp=27744568750&partnerID=8YFLogxK

U2 - 10.1111/j.1751-908X.2004.tb00760.x

DO - 10.1111/j.1751-908X.2004.tb00760.x

M3 - Journal article

AN - SCOPUS:27744568750

VL - 28

SP - 417

EP - 429

JO - Geostandards and Geoanalytical Research

JF - Geostandards and Geoanalytical Research

SN - 1639-4488

IS - 3

ER -

ID: 208729635