Carbonatites, a possible source of scandium as indicated by Sc mineralization in the Fen paralkaline complex, southern Norway-Reference-Cited by-同舟云学术

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Carbonatites, a possible source of scandium as indicated by Sc mineralization in the Fen paralkaline complex, southern Norway

Published:1977-08-01 Issue:5 Volume:72 Page:855-859
ISSN:1554-0774
Container-title:Economic Geology
language:en
Short-container-title:

Author:

Amli R.

Publisher

Society of Economic Geologists

Subject

Economic Geology,Geochemistry and Petrology,Geology,Geophysics

Link

http://pubs.geoscienceworld.org/economicgeology/article-pdf/72/5/855/3485966/855.pdf

Cited by 14 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Trace element minerals from carbonatite-related fluids, The Aird, Scotland;Scottish Journal of Geology;2023-07-07

2. Scandium distribution in the world-class Li-Sn-W Cínovec greisen-type deposit: Result of a complex magmatic to hydrothermal evolution, implications for scandium valorization;Ore Geology Reviews;2021-12

3. Petrography, geochemistry, and geochronology of the Sc-enriched Kiviniemi ferrodiorite intrusion, eastern Finland;Mineralium Deposita;2020-01-23

4. Scandium;Encyclopedia of Earth Sciences Series;2018

5. Scandium;Encyclopedia of Earth Sciences Series;2016

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