A study on a natural pyrite sample as a potential reference material for simultaneous measurement of sulfur and iron isotopes using fs-LA-MC-ICP-MSs-Reference-Cited by-同舟云学术

A study on a natural pyrite sample as a potential reference material for simultaneous measurement of sulfur and iron isotopes using fs-LA-MC-ICP-MSs

Published:2024 Issue:3 Volume:39 Page:723-734
ISSN:0267-9477
Container-title:Journal of Analytical Atomic Spectrometry
language:en
Short-container-title:J. Anal. At. Spectrom.

Author:

Xie Lie-Wen¹^ORCID,Wang Xiao-Jun²,Yu Hui-Min³^ORCID,Gao Jian-Feng⁴,Xu Lei¹^ORCID,Huang Chao¹^ORCID,Tang Guo-Qiang¹,Mao Qian¹,Feng Lian-Jun¹^ORCID,Yang Yue-Heng¹^ORCID,Wu Shi-Tou¹^ORCID,Wang Hao¹^ORCID

Affiliation:

1. State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, P. O. Box 9825, Beijing 100029, P. R. China

2. State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, P. R. China

3. CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China

4. State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou, China

Abstract

A natural pyrite sample has been meticulously examined and identified as a promising reference material. It is ideally suitable for the simultaneous measurement of S and Fe isotopic compositions in pyrite samples using LA-MC-ICP-MS.

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

National Key Research and Development Program of China

Publisher

Royal Society of Chemistry (RSC)

Link

http://pubs.rsc.org/en/content/articlepdf/2024/JA/D3JA00351E

Reference61 articles.

1. Multiple sulphur and iron isotope composition of detrital pyrite in Archaean sedimentary rocks: A new tool for provenance analysis

2. Abiotic Pyrite Formation Produces a Large Fe Isotope Fractionation

3. Deep abiotic weathering of pyrite

4. Constraints on the coevolution of oxic and sulfidic ocean iron sinks from Archean–Paleoproterozoic iron isotope records

5. Microscale heterogeneity of Fe isotopes in >3.71 Ga banded iron formation from the Isua Greenstone Belt, southwest Greenland

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