U-Pb (LA-SF-ICP-MS) dating and probable provenance of detrital zircons from terrigenous deposits of the Upper Precambrian of the Subpolar Urals
https://doi.org/10.24930/1681-9004-2022-22-6-741-760
Abstract
Research subject. Upper Precambrian metaterrigenous deposits of the northern part of the Lyapinsky anticlinorium in the Subpolar Urals.
Material and methods. From the metaterrigenous rocks of the Upper Precambrian section of different stratigraphic levels, monofractions of zircons were isolated and their optical and isotope-geochronological (U-Pb LA-SF-ICPMS) studies were performed.
Results. Age boundaries of the formation of the Puivinskaya, Khobeinskaya, and Moroinskaya Formations in the Subpolar Urals were specified. A comparison was carried out of age populations of detrital zircons from metaterrigenous deposits of the Subpolar Urals and terrigenous sequences of adjacent regions similar in age. The age boundaries and the proposed location of crystalline complexes, the probable provenance areas of terrigenous material, were established.
Conclusions. The lower age limit of the formation of the basal layers of the Upper Precambrian of the Subpolar Urals does not go beyond the Late Riphean. The north-eastern periphery of the East European Platform, including the Subpolar Urals, in the Late Precambrian belonged to the same continental margin, and the accumulation of the Middle-North Timan and Subpolar Ural Upper Riphean sediments occurred in the common sedimentation basin. The lower age boundary of the formation of the Puivinskaya Formation (about 1000 Ma) determines the probable formation time of the Timan passive margin.
About the Authors
A. M. Pystin
Institute of Geology, Komi Science Center UB RAS
Russian Federation
Russian Federation
54 Pervomaiskaya st., 167982 Syktyvkar
O. V. Grakova
Institute of Geology, Komi Science Center UB RAS
Russian Federation
Russian Federation
54 Pervomaiskaya st., 167982 Syktyvkar
Yu. I. Pystina
Institute of Geology, Komi Science Center UB RAS
Russian Federation
Russian Federation
54 Pervomaiskaya st., 167982 Syktyvkar
E. V. Kushmanova
Institute of Geology, Komi Science Center UB RAS
Russian Federation
Russian Federation
54 Pervomaiskaya st., 167982 Syktyvkar
K. S. Popvasev
Institute of Geology, Komi Science Center UB RAS
Russian Federation
Russian Federation
54 Pervomaiskaya st., 167982 Syktyvkar
I. L. Potapov
Institute of Geology, Komi Science Center UB RAS
Russian Federation
Russian Federation
54 Pervomaiskaya st., 167982 Syktyvkar
V. B. Khubanov
Geological Institute SB RAS
Russian Federation
Russian Federation
6a Sakhyanovskaya st., 670047 Ulan-Ude
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Review
For citations:
Pystin A.M., Grakova O.V., Pystina Yu.I., Kushmanova E.V., Popvasev K.S., Potapov I.L., Khubanov V.B. U-Pb (LA-SF-ICP-MS) dating and probable provenance of detrital zircons from terrigenous deposits of the Upper Precambrian of the Subpolar Urals. LITHOSPHERE (Russia). 2022;22(6):741-760. (In Russ.) https://doi.org/10.24930/1681-9004-2022-22-6-741-760
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