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Mineral and trace element zoning of magnetite–hematite ooids of the Rudnogorskoe iron-oxide deposit at the Tunguska Basin, East Siberia: the development of sedimentary accretion and halmyrolysis–diagenesis model

Crossref DOI link: https://doi.org/10.1007/s00126-025-01394-4

Published Online: 2025-10-11

Published Print: 2026-02

Update policy: https://doi.org/10.1007/springer_crossmark_policy

Authors

Maslennikov, V. V. https://orcid.org/0000-0002-1999-2324
Tseluyko, A. S.

Ayupova, N. R.

Artemyev, D. A.
Funding

Funding for this research was provided by:

Russian Science Foundation (22-17-00215)

South Urals Federal Research Centre of Mineralogy and Geoecology UB RAS (№ 075-00880-22-00)
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Article History

Received: 21 February 2024

Accepted: 26 August 2025

First Online: 11 October 2025

Declarations

:

: The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

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