Zircon from banded iron formation as a sensitive indicator of its polychronous background: a case study on the Kostomuksha greenstone belt, Karelian Craton, Fennoscandian Shield-Reference-Cited by-同舟云学术

Zircon from banded iron formation as a sensitive indicator of its polychronous background: a case study on the Kostomuksha greenstone belt, Karelian Craton, Fennoscandian Shield

Published:2023-08-27 Issue: Volume: Page:1-13
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Slabunov А.I.¹^ORCID,Kervinen А.V.¹,Nesterova N.S.¹^ORCID,Maksimov О.А.¹,Medvedev P.V.¹^ORCID

Affiliation:

1. Karelian Research Centre, Russian Academy of Sciences, Petrozavodsk, Russia

Funder

Russian Science Foundation

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2023.2248501

Reference82 articles.

1. Correction of common lead in U–Pb analyses that do not report 204Pb

2. Svecofennian Orogen of the Fennoscandian Shield: Compositional and isotopic zoning and its tectonic interpretation

3. SVECOFENNIAN ACREТION OROGEN: MODERN VIEWS ON ITS STRUCTURE AND EVOLUTION

4. Mesoarchaean banded iron formations of the Fennoscandian Shield: new zirconU-Pb (ID-TIMS and SHRIMP-II) isotope ages of noble metal mineralization and Nd-Sr data on whole rocks

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2. Geochemistry and Formation Conditions of Mesoarchean Banded Iron Formations (BIF-1) from the Kostomuksha Greenstone Belt, Karelian Craton;Geochemistry International;2024-03