Diagenetic behavior of rare-earth elements: an example of layered sulfide ores of the Novy Shemur volcanic-hosted massive sulfide deposit, North Urals, Russia
Author:
Funder
Ural Branch, Russian Academy of Sciences
Russian Science Foundation
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s00531-023-02324-3.pdf
Reference84 articles.
1. Abbott AN, Haley BA, McManus J, Reimers CE (2015) The sedimentary flux of dissolved rare earth elements to the ocean. Geochim Cosmochim Acta 154:186–200. https://doi.org/10.1016/j.gca.2015.01.010
2. Allen JRL (1982) Sedimentary structures, their character and physical basis, vol 2. Elsevier Scientific Pub, Amsterdam, p 663
3. Alt JC (1988) Hydrothermal oxide and nontronite deposits on seamounts in the Eastern Pacific. Mar Geol 81:227–239. https://doi.org/10.1016/0025-3227(88)90029-1
4. Ayupova NR, Maslennikov VV, Tessalina SG et al (2017) Tube fossils from gossanites of the Urals VHMS deposits, Russia: authigenic mineral assemblages and trace element distributions. Ore Geol Rev 85:107–130. https://doi.org/10.1016/j.oregeorev.2016.08.003
5. Ayupova N, Melekestseva I, Maslennikov V, Sadykov S (2022a) Mineralogy and geochemistry of clastic sulfide ores from the Talgan VHMS deposit, South Urals, Russia: signatures of diagenetic alteration. Ore Geol Rev 144:104839. https://doi.org/10.1016/j.oregeorev.2022.104839
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