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The Provenance of Terrigenous Rocks of the Basal Horizons of the Uralides of the Baidarata Allochthon (Polar Urals) According to the U–Pb Isotope Age of Detrital Zircon. / Sychev, S. N.; Ivleva, A. S.; Petrov, S. Yu.; Petrova, M. N.; Ershova, V. B.; Veselovskiy, R. V.; Konnov, A. G.

In: Moscow University Geology Bulletin, Vol. 72, No. 3, 2017, p. 172-180.

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

Harvard

Sychev, SN, Ivleva, AS, Petrov, SY, Petrova, MN, Ershova, VB, Veselovskiy, RV & Konnov, AG 2017, 'The Provenance of Terrigenous Rocks of the Basal Horizons of the Uralides of the Baidarata Allochthon (Polar Urals) According to the U–Pb Isotope Age of Detrital Zircon', Moscow University Geology Bulletin, vol. 72, no. 3, pp. 172-180. https://doi.org/10.3103/S0145875217030048

APA

Sychev, S. N., Ivleva, A. S., Petrov, S. Y., Petrova, M. N., Ershova, V. B., Veselovskiy, R. V., & Konnov, A. G. (2017). The Provenance of Terrigenous Rocks of the Basal Horizons of the Uralides of the Baidarata Allochthon (Polar Urals) According to the U–Pb Isotope Age of Detrital Zircon. Moscow University Geology Bulletin, 72(3), 172-180. https://doi.org/10.3103/S0145875217030048

Vancouver

Sychev SN, Ivleva AS, Petrov SY, Petrova MN, Ershova VB, Veselovskiy RV et al. The Provenance of Terrigenous Rocks of the Basal Horizons of the Uralides of the Baidarata Allochthon (Polar Urals) According to the U–Pb Isotope Age of Detrital Zircon. Moscow University Geology Bulletin. 2017;72(3):172-180. https://doi.org/10.3103/S0145875217030048

Author

Sychev, S. N. ; Ivleva, A. S. ; Petrov, S. Yu. ; Petrova, M. N. ; Ershova, V. B. ; Veselovskiy, R. V. ; Konnov, A. G. / The Provenance of Terrigenous Rocks of the Basal Horizons of the Uralides of the Baidarata Allochthon (Polar Urals) According to the U–Pb Isotope Age of Detrital Zircon. In: Moscow University Geology Bulletin. 2017 ; Vol. 72, No. 3. pp. 172-180.

BibTeX

@article{acd4e735bdc148bbac02222a79fa965d,
title = "The Provenance of Terrigenous Rocks of the Basal Horizons of the Uralides of the Baidarata Allochthon (Polar Urals) According to the U–Pb Isotope Age of Detrital Zircon",
abstract = "The U–Pb (LA–ICP–MS) age of detrital zircons from the Upper Cambrian–Lower Ordovician terrigenous rocks of the Baidarata Allochthon, which is located in the northern part of the Polar Urals, is determined. The analysis of the youngest zircon population indicates a broad occurrence of the Uralides in this area rather than Pre-Uralides, as was considered previously. The Bedamel island-arc rocks (rather than Timan orogen) were probably the major provenance for the studied sequences. The results of statistical processing of the U–Pb ages of zircons from coeval rocks of Arctic regions suggest similar provenances for the Baidarata Allochthon and Novaya Zemlya and Severnaya Zemlya archipelagoes.",
author = "Sychev, {S. N.} and Ivleva, {A. S.} and Petrov, {S. Yu.} and Petrova, {M. N.} and Ershova, {V. B.} and Veselovskiy, {R. V.} and Konnov, {A. G.}",
year = "2017",
doi = "10.3103/S0145875217030048",
language = "English",
volume = "72",
pages = "172--180",
journal = "Moscow University Geology Bulletin",
issn = "0145-8752",
publisher = "Springer Nature",
number = "3",

}

RIS

TY - JOUR

T1 - The Provenance of Terrigenous Rocks of the Basal Horizons of the Uralides of the Baidarata Allochthon (Polar Urals) According to the U–Pb Isotope Age of Detrital Zircon

AU - Sychev, S. N.

AU - Ivleva, A. S.

AU - Petrov, S. Yu.

AU - Petrova, M. N.

AU - Ershova, V. B.

AU - Veselovskiy, R. V.

AU - Konnov, A. G.

PY - 2017

Y1 - 2017

N2 - The U–Pb (LA–ICP–MS) age of detrital zircons from the Upper Cambrian–Lower Ordovician terrigenous rocks of the Baidarata Allochthon, which is located in the northern part of the Polar Urals, is determined. The analysis of the youngest zircon population indicates a broad occurrence of the Uralides in this area rather than Pre-Uralides, as was considered previously. The Bedamel island-arc rocks (rather than Timan orogen) were probably the major provenance for the studied sequences. The results of statistical processing of the U–Pb ages of zircons from coeval rocks of Arctic regions suggest similar provenances for the Baidarata Allochthon and Novaya Zemlya and Severnaya Zemlya archipelagoes.

AB - The U–Pb (LA–ICP–MS) age of detrital zircons from the Upper Cambrian–Lower Ordovician terrigenous rocks of the Baidarata Allochthon, which is located in the northern part of the Polar Urals, is determined. The analysis of the youngest zircon population indicates a broad occurrence of the Uralides in this area rather than Pre-Uralides, as was considered previously. The Bedamel island-arc rocks (rather than Timan orogen) were probably the major provenance for the studied sequences. The results of statistical processing of the U–Pb ages of zircons from coeval rocks of Arctic regions suggest similar provenances for the Baidarata Allochthon and Novaya Zemlya and Severnaya Zemlya archipelagoes.

U2 - 10.3103/S0145875217030048

DO - 10.3103/S0145875217030048

M3 - Article

VL - 72

SP - 172

EP - 180

JO - Moscow University Geology Bulletin

JF - Moscow University Geology Bulletin

SN - 0145-8752

IS - 3

ER -

ID: 33296063