Geochemistry and age of detrital zircon from the Quaternary deposits from the Ufaley block (Middle Urals): provenance and the problem of Precambrian
https://doi.org/10.24930/1681-9004-2025-25-4-819-847
EDN: TXPUTT
Abstract
Research subject. Detrital zircons from the Quaternary deposits from the frame of pyroxenite composing the Shigirsky hills in the western part of the Ufaley block.
Aim. The verification of the Pre-Cambrian dating, evaluation of the substrate type and geotectonic settings of rocks enclosing ultramafites of the Ufaley block.
Materials and methods. U-Pb isotope dating and determination of rare and rare-earth elements in detrital zircon by laser ablation, RSMA investigation of minerals, establishing of zircon nature and provenance and the distance of zircon migration.
Results. Dominant Paleoproterozoic (2100–2000 Ma) maximum for the distribution of detrital zircon age accompanied by lower picks of the Archean and Neoproterozoic-Lower Ordovician age has been established. Detrital zircon was derived from continental-type sources corresponding to igneous and metamorphic rocks of basic, intermediate and acidic composition. The transfer distance was negligible.
Conclusions. Zircon morphology, its internal structure, mineral inclusions, geochemistry and age allow to suggests the similar protolith and joint the Precambrian evolution at least the western part of the Ufaley block and Taratash and Alexandrovsky blocks, which are the fragments of crystalline complexes of the Archean Volga-Uraliya craton. This conclusion supports additionally by similarity in composition of high-Ca mafic-ultramafic rocks known in these blocks.
Keywords
detrital zircon,
protolith,
provenance,
isotope dating,
geochemistry,
Proterozoic,
continental crust,
ultramafic and basic rocks,
the Ufaley block,
Urals
Supporting agencies: This work was conducted with financial support from the Russian Foundation for Basic Research, grant No. 23-17-00224. https://rscf.ru/project/23-17-00224.
About the Authors
G. Y. Shardakova
A.N. Zavaritsky Institute of Geology and Geochemistry, UB RAS
Russian Federation
Russian Federation
Galina Y. Shardakova
15 Academician Vonsovsky st., Ekaterinburg 620110
E. V. Pushkarev
A.N. Zavaritsky Institute of Geology and Geochemistry, UB RAS
Russian Federation
Russian Federation
Evgenii V. Pushkarev
15 Academician Vonsovsky st., Ekaterinburg 620110
A. O. Simankova
A.N. Zavaritsky Institute of Geology and Geochemistry, UB RAS
Russian Federation
Russian Federation
Aleksandra O. Simankova
15 Academician Vonsovsky st., Ekaterinburg 620110
V. S. Chervyakovsky
A.N. Zavaritsky Institute of Geology and Geochemistry, UB RAS
Russian Federation
Russian Federation
Vasiliy S. Chervyakovsky
15 Academician Vonsovsky st., Ekaterinburg 620110
M. V. Chervyakovskaya
A.N. Zavaritsky Institute of Geology and Geochemistry, UB RAS
Russian Federation
Russian Federation
Maria V. Chervyakovskaya
15 Academician Vonsovsky st., Ekaterinburg 620110
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Shardakova G.Y., Pushkarev E.V., Simankova A.O., Chervyakovsky V.S., Chervyakovskaya M.V. Geochemistry and age of detrital zircon from the Quaternary deposits from the Ufaley block (Middle Urals): provenance and the problem of Precambrian. LITHOSPHERE (Russia). 2025;25(4):819-847. (In Russ.) https://doi.org/10.24930/1681-9004-2025-25-4-819-847. EDN: TXPUTT
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