Trace element analysis of high-Mg olivine by LA-ICP-MS - Characterization of natural olivine standards for matrix-matched calibration and application to mantle peridotites

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Standard

Trace element analysis of high-Mg olivine by LA-ICP-MS - Characterization of natural olivine standards for matrix-matched calibration and application to mantle peridotites. / Bussweiler, Y.; Giuliani, A.; Greig, A.; Kjarsgaard, B. A.; Petts, D.; Barrett, N.; Pearson, D. G.

I: Chemical Geology, Bind 524, 05.10.2019, s. 136-157.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Bussweiler, Y, Giuliani, A, Greig, A, Kjarsgaard, BA, Petts, D, Barrett, N & Pearson, DG 2019, 'Trace element analysis of high-Mg olivine by LA-ICP-MS - Characterization of natural olivine standards for matrix-matched calibration and application to mantle peridotites', Chemical Geology, bind 524, s. 136-157. https://doi.org/10.1016/j.chemgeo.2019.06.019

APA

Bussweiler, Y., Giuliani, A., Greig, A., Kjarsgaard, B. A., Petts, D., Barrett, N., & Pearson, D. G. (2019). Trace element analysis of high-Mg olivine by LA-ICP-MS - Characterization of natural olivine standards for matrix-matched calibration and application to mantle peridotites. Chemical Geology, 524, 136-157. https://doi.org/10.1016/j.chemgeo.2019.06.019

Vancouver

Bussweiler Y, Giuliani A, Greig A, Kjarsgaard BA, Petts D, Barrett N o.a. Trace element analysis of high-Mg olivine by LA-ICP-MS - Characterization of natural olivine standards for matrix-matched calibration and application to mantle peridotites. Chemical Geology. 2019 okt. 5;524:136-157. https://doi.org/10.1016/j.chemgeo.2019.06.019

Author

Bussweiler, Y. ; Giuliani, A. ; Greig, A. ; Kjarsgaard, B. A. ; Petts, D. ; Barrett, N. ; Pearson, D. G. / Trace element analysis of high-Mg olivine by LA-ICP-MS - Characterization of natural olivine standards for matrix-matched calibration and application to mantle peridotites. I: Chemical Geology. 2019 ; Bind 524. s. 136-157.

Bibtex

@article{ed113177a7804e329933b4c601927d82,
title = "Trace element analysis of high-Mg olivine by LA-ICP-MS - Characterization of natural olivine standards for matrix-matched calibration and application to mantle peridotites",
abstract = "The trace element composition of olivine is becoming increasingly important in petrological studies due to the ubiquity of olivine in the Earths upper mantle and in primitive magmatic rocks. The LA-ICP-MS method allows for the routine analysis of trace elements in olivine to sub-ppm levels, but a major drawback of this method is the lack of knowledge about possible downhole fractionation effects when non matrix-matched calibration is used. In this contribution, we show that matrix-matched (i.e., olivine-based) calibration is preferable for small laser spot sizes (= 100 mu m, laser fluence of",
keywords = "Olivine, Mantle peridotite, Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS), Elemental fractionation, Downhole fractionation, Matrix effects, INDUCTIVELY-COUPLED-PLASMA, 193 NM, INCLUSIONS, ORIGIN, ROCKS, METASOMATISM, KIMBERLEY, GLASSES, VALUES, FLUID",
author = "Y. Bussweiler and A. Giuliani and A. Greig and Kjarsgaard, {B. A.} and D. Petts and N. Barrett and Pearson, {D. G.}",
year = "2019",
month = oct,
day = "5",
doi = "10.1016/j.chemgeo.2019.06.019",
language = "English",
volume = "524",
pages = "136--157",
journal = "Chemical Geology",
issn = "0009-2541",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Trace element analysis of high-Mg olivine by LA-ICP-MS - Characterization of natural olivine standards for matrix-matched calibration and application to mantle peridotites

AU - Bussweiler, Y.

AU - Giuliani, A.

AU - Greig, A.

AU - Kjarsgaard, B. A.

AU - Petts, D.

AU - Barrett, N.

AU - Pearson, D. G.

PY - 2019/10/5

Y1 - 2019/10/5

N2 - The trace element composition of olivine is becoming increasingly important in petrological studies due to the ubiquity of olivine in the Earths upper mantle and in primitive magmatic rocks. The LA-ICP-MS method allows for the routine analysis of trace elements in olivine to sub-ppm levels, but a major drawback of this method is the lack of knowledge about possible downhole fractionation effects when non matrix-matched calibration is used. In this contribution, we show that matrix-matched (i.e., olivine-based) calibration is preferable for small laser spot sizes (= 100 mu m, laser fluence of

AB - The trace element composition of olivine is becoming increasingly important in petrological studies due to the ubiquity of olivine in the Earths upper mantle and in primitive magmatic rocks. The LA-ICP-MS method allows for the routine analysis of trace elements in olivine to sub-ppm levels, but a major drawback of this method is the lack of knowledge about possible downhole fractionation effects when non matrix-matched calibration is used. In this contribution, we show that matrix-matched (i.e., olivine-based) calibration is preferable for small laser spot sizes (= 100 mu m, laser fluence of

KW - Olivine

KW - Mantle peridotite

KW - Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS)

KW - Elemental fractionation

KW - Downhole fractionation

KW - Matrix effects

KW - INDUCTIVELY-COUPLED-PLASMA

KW - 193 NM

KW - INCLUSIONS

KW - ORIGIN

KW - ROCKS

KW - METASOMATISM

KW - KIMBERLEY

KW - GLASSES

KW - VALUES

KW - FLUID

U2 - 10.1016/j.chemgeo.2019.06.019

DO - 10.1016/j.chemgeo.2019.06.019

M3 - Journal article

VL - 524

SP - 136

EP - 157

JO - Chemical Geology

JF - Chemical Geology

SN - 0009-2541

ER -

ID: 335709074