Heavy rare earth element and crustal-derived silicon enrichment in Huayangchuan carbonatites, Qinling orogenic belt-Reference-Cited by-同舟云学术

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Heavy rare earth element and crustal-derived silicon enrichment in Huayangchuan carbonatites, Qinling orogenic belt

Published:2023-01 Issue: Volume:436-437 Page:106987
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Wei Chun-wan,Xu Cheng,Song Wen-lei,Chen Wei,Shi Aiguo,Li Zhuoqi,Fan Chaoxi

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference92 articles.

1. Experimentally determined partition coefficients for minor and trace elements in peridotite minerals and carbonatitic melt, and their relevance to natural carbonatites;Adam;Eur. J. Mineral.,2001

2. Deciphering igneous and metamorphic events in high-grade rocks of the Wilmington complex, Delaware: Morphology, cathodoluminescence and backscattered electron zoning, and SHRIMP U-Pb geochronology of zircon and monazite;Aleinikoff;GSA Bull.,2006

3. Carbonatitic versus hydrothermal origin for fluorapatite REE-Th deposits: Experimental study of REE transport and crustal “antiskarn” metasomatism;Anenburg;Am. J. Sci.,2018

4. The Fluorapatite P–REE–Th Vein Deposit at Nolans Bore: Genesis by Carbonatite Metasomatism;Anenburg;J. Petrol.,2020

5. Rare earth element mobility in and around carbonatites controlled by sodium, potassium, and silica;Anenburg;Sci. Adv.,2020

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1. Laser ablation (in situ) Lu-Hf geochronology of epidote group minerals;Contributions to Mineralogy and Petrology;2024-05-25

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