A mineral formula-based calibration method for major and trace element determination of mica without applying an internal element by LA-ICP-MS-Reference-Cited by-同舟云学术

A mineral formula-based calibration method for major and trace element determination of mica without applying an internal element by LA-ICP-MS

Published:2023 Issue:7 Volume:38 Page:1387-1393
ISSN:0267-9477
Container-title:Journal of Analytical Atomic Spectrometry
language:en
Short-container-title:J. Anal. At. Spectrom.

Author:

Zhang Hao-Xiang¹,Jiang Shao-Yong¹²^ORCID,Su Hui-Min¹,Li Wen-Tian¹,Liu Si-Qi¹,Che Yu-Ying¹

Affiliation:

1. State Key Laboratory of Geological Processes and Mineral Resources, Collaborative Innovation Center for Exploration of Strategic Mineral Resources, School of Earth Resources, China University of Geosciences, Wuhan, 430074, P. R. China

2. Key Laboratory of Geological Survey and Evaluation of Ministry of Education, China University of Geosciences, Wuhan, 430074, P. R. China

Abstract

Accurate determination for most major and trace elements in mica with 5% relative deviation and relative standard deviation is achieved by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) without an internal standard.

Funder

National Natural Science Foundation of China

State Key Laboratory of Geological Processes and Mineral Resources

Publisher

Royal Society of Chemistry (RSC)

Subject

Spectroscopy,Analytical Chemistry

Link

http://pubs.rsc.org/en/content/articlepdf/2023/JA/D3JA00026E

Reference14 articles.

1. The key role of mica during igneous concentration of tantalum

2. Episodic hydrothermal alteration recorded by microscale oxygen isotope analysis of white mica in the Larderello-Travale Geothermal Field, Italy

3. Critical metal enrichment in crustal melts: The role of metamorphic mica

4. Alkali metal and rare earth element evolution of rock-forming minerals from the Gatumba area pegmatites (Rwanda): Quantitative assessment of crystal-melt fractionation in the regional zonation of pegmatite groups

5. Mica-liquid trace elements partitioning and the granite-pegmatite connection: The St-Sylvestre complex (Western French Massif Central)

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