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Age and provenance of the Precambrian Middle Timan clastic succession : Constraints from detrital zircon and rutile studies. / Brustnitsyna, Ekaterina; Ershova, Victoria; Khudoley, Andrei; Maslov, Andrei; Andersen, Tom; Stockli, Daniel; Kristoffersen, Magnus.

In: Precambrian Research, Vol. 371, 106580, 04.2022.

Research output: Contribution to journal › Article › peer-review

Harvard

Brustnitsyna, E, Ershova, V, Khudoley, A, Maslov, A, Andersen, T, Stockli, D & Kristoffersen, M 2022, 'Age and provenance of the Precambrian Middle Timan clastic succession: Constraints from detrital zircon and rutile studies', Precambrian Research, vol. 371, 106580. https://doi.org/10.1016/j.precamres.2022.106580

APA

Brustnitsyna, E., Ershova, V., Khudoley, A., Maslov, A., Andersen, T., Stockli, D., & Kristoffersen, M. (2022). Age and provenance of the Precambrian Middle Timan clastic succession: Constraints from detrital zircon and rutile studies. Precambrian Research, 371, [106580]. https://doi.org/10.1016/j.precamres.2022.106580

Vancouver

Brustnitsyna E, Ershova V, Khudoley A, Maslov A, Andersen T, Stockli D et al. Age and provenance of the Precambrian Middle Timan clastic succession: Constraints from detrital zircon and rutile studies. Precambrian Research. 2022 Apr;371. 106580. https://doi.org/10.1016/j.precamres.2022.106580

Author

Brustnitsyna, Ekaterina ; Ershova, Victoria ; Khudoley, Andrei ; Maslov, Andrei ; Andersen, Tom ; Stockli, Daniel ; Kristoffersen, Magnus. / Age and provenance of the Precambrian Middle Timan clastic succession : Constraints from detrital zircon and rutile studies. In: Precambrian Research. 2022 ; Vol. 371.

BibTeX

@article{4190050f4e134e29b665bf47ae8b45b9,
title = "Age and provenance of the Precambrian Middle Timan clastic succession: Constraints from detrital zircon and rutile studies",
abstract = "The Precambrian sedimentary succession of Middle Timan provides important information on the coeval history of Baltica prior to assembly of the Rodinia supercontinent. This study comprises a comprehensive integrated provenance study based on samples collected from Precambrian clastic rocks of the Chetlassky Kamen and Volsko-Vymskaya Ridge. The maximum depositional age of the studied succession is constrained as latest Mesoproterozoic – earliest Neoproterozoic based on the youngest detrital zircon and rutile ages. Metasandstone samples within the succession are arkose, sublitharenite and litharenite. The distributions of detrital zircon U-Pb ages from the studied metasedimentary rocks are very comparable, yielding approximately 50% Mesoproterozoic ages within the ranges 1470 – 1550 and 1170 – 1370 Ma, 45% Paleoproterozoic ages and 5% Archean ages, with predominant populations grouping at 2500–2700 and 1800–1900 Ma. Comparable detrital zircon age distributions within the coeval strata of northern Baltica suggest a common provenance area. Analysis of detrital rutile suggests the widespread distribution of latest Mesoproterozoic – earliest Neoproterozoic metamorphism within the provenance area. A comparison of detrital zircon age distributions from the coeval strata of Baltica and Laurentia also revealed a striking similarity. Therefore, we suggest that clasts were in fact predominantly sourced from the Grenvillian-Sveconorwegian Orogen, with possible reworking of older zircon grains from older sedimentary rocks involved in the deformation and uplift. Our data support the tectonic model invoking a continuation of the Grenvillian-Sveconorwegian Orogen further to the east across the Barents Sea from its closest modern outcrop in Scandinavia.",
keywords = "Baltica, Detrital rutile, Detrital zircon, Grenvillian-Sveconorwegian Orogen, Mesoproterozoic, Middle Timan, Neoproterozoic",
author = "Ekaterina Brustnitsyna and Victoria Ershova and Andrei Khudoley and Andrei Maslov and Tom Andersen and Daniel Stockli and Magnus Kristoffersen",
note = "Publisher Copyright: {\textcopyright} 2022 Elsevier B.V.",
year = "2022",
month = apr,
doi = "10.1016/j.precamres.2022.106580",
language = "English",
volume = "371",
journal = "Precambrian Research",
issn = "0301-9268",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Age and provenance of the Precambrian Middle Timan clastic succession

T2 - Constraints from detrital zircon and rutile studies

AU - Brustnitsyna, Ekaterina

AU - Ershova, Victoria

AU - Khudoley, Andrei

AU - Maslov, Andrei

AU - Andersen, Tom

AU - Stockli, Daniel

AU - Kristoffersen, Magnus

N1 - Publisher Copyright: © 2022 Elsevier B.V.

PY - 2022/4

Y1 - 2022/4

N2 - The Precambrian sedimentary succession of Middle Timan provides important information on the coeval history of Baltica prior to assembly of the Rodinia supercontinent. This study comprises a comprehensive integrated provenance study based on samples collected from Precambrian clastic rocks of the Chetlassky Kamen and Volsko-Vymskaya Ridge. The maximum depositional age of the studied succession is constrained as latest Mesoproterozoic – earliest Neoproterozoic based on the youngest detrital zircon and rutile ages. Metasandstone samples within the succession are arkose, sublitharenite and litharenite. The distributions of detrital zircon U-Pb ages from the studied metasedimentary rocks are very comparable, yielding approximately 50% Mesoproterozoic ages within the ranges 1470 – 1550 and 1170 – 1370 Ma, 45% Paleoproterozoic ages and 5% Archean ages, with predominant populations grouping at 2500–2700 and 1800–1900 Ma. Comparable detrital zircon age distributions within the coeval strata of northern Baltica suggest a common provenance area. Analysis of detrital rutile suggests the widespread distribution of latest Mesoproterozoic – earliest Neoproterozoic metamorphism within the provenance area. A comparison of detrital zircon age distributions from the coeval strata of Baltica and Laurentia also revealed a striking similarity. Therefore, we suggest that clasts were in fact predominantly sourced from the Grenvillian-Sveconorwegian Orogen, with possible reworking of older zircon grains from older sedimentary rocks involved in the deformation and uplift. Our data support the tectonic model invoking a continuation of the Grenvillian-Sveconorwegian Orogen further to the east across the Barents Sea from its closest modern outcrop in Scandinavia.

AB - The Precambrian sedimentary succession of Middle Timan provides important information on the coeval history of Baltica prior to assembly of the Rodinia supercontinent. This study comprises a comprehensive integrated provenance study based on samples collected from Precambrian clastic rocks of the Chetlassky Kamen and Volsko-Vymskaya Ridge. The maximum depositional age of the studied succession is constrained as latest Mesoproterozoic – earliest Neoproterozoic based on the youngest detrital zircon and rutile ages. Metasandstone samples within the succession are arkose, sublitharenite and litharenite. The distributions of detrital zircon U-Pb ages from the studied metasedimentary rocks are very comparable, yielding approximately 50% Mesoproterozoic ages within the ranges 1470 – 1550 and 1170 – 1370 Ma, 45% Paleoproterozoic ages and 5% Archean ages, with predominant populations grouping at 2500–2700 and 1800–1900 Ma. Comparable detrital zircon age distributions within the coeval strata of northern Baltica suggest a common provenance area. Analysis of detrital rutile suggests the widespread distribution of latest Mesoproterozoic – earliest Neoproterozoic metamorphism within the provenance area. A comparison of detrital zircon age distributions from the coeval strata of Baltica and Laurentia also revealed a striking similarity. Therefore, we suggest that clasts were in fact predominantly sourced from the Grenvillian-Sveconorwegian Orogen, with possible reworking of older zircon grains from older sedimentary rocks involved in the deformation and uplift. Our data support the tectonic model invoking a continuation of the Grenvillian-Sveconorwegian Orogen further to the east across the Barents Sea from its closest modern outcrop in Scandinavia.

KW - Baltica

KW - Detrital rutile

KW - Detrital zircon

KW - Grenvillian-Sveconorwegian Orogen

KW - Mesoproterozoic

KW - Middle Timan

KW - Neoproterozoic

UR - http://www.scopus.com/inward/record.url?scp=85124593625&partnerID=8YFLogxK

UR - https://www.mendeley.com/catalogue/0110b943-6493-3703-8a9b-3f2e6bfa9a31/

U2 - 10.1016/j.precamres.2022.106580

DO - 10.1016/j.precamres.2022.106580

M3 - Article

AN - SCOPUS:85124593625

VL - 371

JO - Precambrian Research

JF - Precambrian Research

SN - 0301-9268

M1 - 106580

ER -

ID: 94128062