Research output: Contribution to journal › Article › peer-review
Maximum Depositional Age of Pre-Middle Paleozoic Terrigenous Rocks of the Vychegda Trough (Northeast of the East European Platform): Results of U–Pb Dating of Detrital Zircons. / Ershova, V.B.; Podkovyrov, V.N.; Ivleva, A.S.; Maslov, A.V.
In: Doklady Earth Sciences, Vol. 524, No. 2, 21.09.2025.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Maximum Depositional Age of Pre-Middle Paleozoic Terrigenous Rocks of the Vychegda Trough (Northeast of the East European Platform): Results of U–Pb Dating of Detrital Zircons
AU - Ershova, V.B.
AU - Podkovyrov, V.N.
AU - Ivleva, A.S.
AU - Maslov, A.V.
N1 - Export Date: 01 November 2025; Cited By: 0; Correspondence Address: V.B. Ershova; St. Petersburg State University, St. Petersburg, 199034, Russian Federation; email: ershovavictoria@gmail.com; V.N. Podkovyrov; Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, St. Petersburg, 199034, Russian Federation; email: vpodk@mail.ru
PY - 2025/9/21
Y1 - 2025/9/21
N2 - Abstract: U–Pb dating (LA-ICP-MS) is carried out on detrital zircon from pre-Middle Devonian terrigenous deposits of the Vychegda Trough (southern margin of the Mezen syneclise) penetrated by Seregovo 1, Storozhevsk 1, and Keltma 1 parametric wells. Analysis of the detrital zircon ages and subsequent calculations of maximum depositional age (MDA) based on different algorithms has made it possible to clarify the stratigraphic position of the studied successions. The deposits of the Nyafta Formation, penetrated by Seregovo 1 well, have Middle Riphean MDAs. The MDAs of the Uftyug Formation zircons correspond to the Middle-Late Riphean, and those of the Ust-Pinega Formation correspond to the Late Riphean. For the Mezen Formation, penetrated by Keltma 1 well, the calculated MDAs for the first time suggest an Early Cambrian or younger age. © 2025 Elsevier B.V., All rights reserved.
AB - Abstract: U–Pb dating (LA-ICP-MS) is carried out on detrital zircon from pre-Middle Devonian terrigenous deposits of the Vychegda Trough (southern margin of the Mezen syneclise) penetrated by Seregovo 1, Storozhevsk 1, and Keltma 1 parametric wells. Analysis of the detrital zircon ages and subsequent calculations of maximum depositional age (MDA) based on different algorithms has made it possible to clarify the stratigraphic position of the studied successions. The deposits of the Nyafta Formation, penetrated by Seregovo 1 well, have Middle Riphean MDAs. The MDAs of the Uftyug Formation zircons correspond to the Middle-Late Riphean, and those of the Ust-Pinega Formation correspond to the Late Riphean. For the Mezen Formation, penetrated by Keltma 1 well, the calculated MDAs for the first time suggest an Early Cambrian or younger age. © 2025 Elsevier B.V., All rights reserved.
KW - Cambrian
KW - detrital zircon
KW - stratigraphy
KW - Vendian
KW - Vychegda Trough
KW - Deposits
KW - Geochronology
KW - Zircon
KW - Zircon deposits
KW - Cambrians
KW - Detrital zircon
KW - European Platform
KW - Middle Devonian
KW - Paleozoic
KW - Riphean
KW - U-Pb dating
KW - Vychegda trough
KW - Zircon age
KW - Stratigraphy
KW - algorithm
KW - deposition
KW - detrital deposit
KW - formation mechanism
KW - geochronology
KW - uranium-lead dating
KW - zircon
KW - Russian Platform
UR - https://www.mendeley.com/catalogue/8d1bc685-b682-3138-b99d-fc168039e492/
U2 - 10.1134/s1028334x25607163
DO - 10.1134/s1028334x25607163
M3 - статья
VL - 524
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 2
ER -
ID: 143730995