Non-matrix-matched analysis of Fe isotopes in silicates by laser ablation MC-ICP-MS and potential silicate in-house standards for microbeam Fe isotopic analysis-Reference-Cited by-同舟云学术

Non-matrix-matched analysis of Fe isotopes in silicates by laser ablation MC-ICP-MS and potential silicate in-house standards for microbeam Fe isotopic analysis

Published:2024 Issue:3 Volume:39 Page:900-916
ISSN:0267-9477
Container-title:Journal of Analytical Atomic Spectrometry
language:en
Short-container-title:J. Anal. At. Spectrom.

Author:

Xu Lei¹²^ORCID,Yang Jin-Hui¹²³,Wang Hao¹²³^ORCID,Ye Hui⁴,Xie Lie-Wen¹²,Yang Yue-Heng¹²^ORCID,Huang Chao¹²^ORCID,Wu Shi-Tou¹²^ORCID

Affiliation:

1. State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

2. Innovation Academy of Earth Science, Chinese Academy of Sciences, Beijing 100029, China

3. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China

4. MOE Key Laboratory of Western China's Mineral Resources and Geological Engineering, School of Earth Science and Resources, Chang'an University, Xi'an, 710054, China

Abstract

Fe isotopic compositions of natural silicate minerals, including olivine, garnet, amphibole and biotite are directly calibrated against non-matrix-matched BCR-2G glass by LA-MC-ICP-MS under wet plasma conditions.

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

Publisher

Royal Society of Chemistry (RSC)

Link

http://pubs.rsc.org/en/content/articlepdf/2024/JA/D3JA00364G

Reference59 articles.

1. Partial melting and melt percolation in the mantle: The message from Fe isotopes

2. Iron isotopes may reveal the redox conditions of mantle melting from Archean to Present

3. Iron, zinc, magnesium and uranium isotopic fractionation during continental crust differentiation: The tale from migmatites, granitoids, and pegmatites

4. Iron, magnesium, and titanium isotopic fractionations between garnet, ilmenite, fayalite, biotite, and tourmaline: Results from NRIXS, ab initio, and study of mineral separates from the Moosilauke metapelite

5. Iron Isotope Biosignatures