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Early Carboniferous paleogeography of the northern Verkhoyansk passive margin as derived from U-Pb dating of detrital zircons: Role of erosion products of the Central Asian and Taimyr-Severnaya Zemlya fold belts11The article was translated by the authors. / Prokopiev, A.V.; Ershova, V.B.; Miller, E.L.; Khudoley, A.K.

в: Russian Geology and Geophysics, № 10, 2013, стр. 1195-1204.

Результаты исследований: Научные публикации в периодических изданиях › статья

Harvard

Prokopiev, AV, Ershova, VB, Miller, EL & Khudoley, AK 2013, 'Early Carboniferous paleogeography of the northern Verkhoyansk passive margin as derived from U-Pb dating of detrital zircons: Role of erosion products of the Central Asian and Taimyr-Severnaya Zemlya fold belts11The article was translated by the authors.', Russian Geology and Geophysics, № 10, стр. 1195-1204. https://doi.org/10.1016/j.rgg.2013.09.005

APA

Prokopiev, A. V., Ershova, V. B., Miller, E. L., & Khudoley, A. K. (2013). Early Carboniferous paleogeography of the northern Verkhoyansk passive margin as derived from U-Pb dating of detrital zircons: Role of erosion products of the Central Asian and Taimyr-Severnaya Zemlya fold belts11The article was translated by the authors. Russian Geology and Geophysics, (10), 1195-1204. https://doi.org/10.1016/j.rgg.2013.09.005

Vancouver

Prokopiev AV, Ershova VB, Miller EL, Khudoley AK. Early Carboniferous paleogeography of the northern Verkhoyansk passive margin as derived from U-Pb dating of detrital zircons: Role of erosion products of the Central Asian and Taimyr-Severnaya Zemlya fold belts11The article was translated by the authors. Russian Geology and Geophysics. 2013;(10):1195-1204. https://doi.org/10.1016/j.rgg.2013.09.005

Author

Prokopiev, A.V. ; Ershova, V.B. ; Miller, E.L. ; Khudoley, A.K. / Early Carboniferous paleogeography of the northern Verkhoyansk passive margin as derived from U-Pb dating of detrital zircons: Role of erosion products of the Central Asian and Taimyr-Severnaya Zemlya fold belts11The article was translated by the authors. в: Russian Geology and Geophysics. 2013 ; № 10. стр. 1195-1204.

BibTeX

@article{277697cd47ce4a8aabb68f29c1d8d7f8,
title = "Early Carboniferous paleogeography of the northern Verkhoyansk passive margin as derived from U-Pb dating of detrital zircons: Role of erosion products of the Central Asian and Taimyr-Severnaya Zemlya fold belts11The article was translated by the authors.",
abstract = "The first U-Pb dating of detrital zircons from the Lower Carboniferous sandstones in the frontal part of the northern Verkhoyansk fold-and-thrust belt showed that detrital zircon age spectra for the Lower Visean (Krestyakh Formation) and the Upper Visean-Serpukhovian (Tiksi Formation) rocks are quite different. The Early Visean sandstones contain up to 95% detrital zircons of Precambrian age, while those of Late Visean-Serpukhovian age, only 55%. The shape of age distribution plots of Precambrian zircons for both samples is similar, indicating that reworking of terrigenous sediments of the Krestyakh Formation or the same sources dominated in Early Visean time (crystalline basement of the craton, eroded Meso-and Neoproterozoic sedimentary complexes, and igneous rocks of Central Taimyr) contributed significantly to the accumulation of the Late Visean-Serpukhovian deposits. In the rocks of the Tiksi Formation, 45% of detrital zircons are of Paleozoic age, while 24% are Early Paleozoic, with prevailing Cambrian a",
author = "A.V. Prokopiev and V.B. Ershova and E.L. Miller and A.K. Khudoley",
year = "2013",
doi = "10.1016/j.rgg.2013.09.005",
language = "English",
pages = "1195--1204",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier",
number = "10",

}

RIS

TY - JOUR

T1 - Early Carboniferous paleogeography of the northern Verkhoyansk passive margin as derived from U-Pb dating of detrital zircons: Role of erosion products of the Central Asian and Taimyr-Severnaya Zemlya fold belts11The article was translated by the authors.

AU - Prokopiev, A.V.

AU - Ershova, V.B.

AU - Miller, E.L.

AU - Khudoley, A.K.

PY - 2013

Y1 - 2013

N2 - The first U-Pb dating of detrital zircons from the Lower Carboniferous sandstones in the frontal part of the northern Verkhoyansk fold-and-thrust belt showed that detrital zircon age spectra for the Lower Visean (Krestyakh Formation) and the Upper Visean-Serpukhovian (Tiksi Formation) rocks are quite different. The Early Visean sandstones contain up to 95% detrital zircons of Precambrian age, while those of Late Visean-Serpukhovian age, only 55%. The shape of age distribution plots of Precambrian zircons for both samples is similar, indicating that reworking of terrigenous sediments of the Krestyakh Formation or the same sources dominated in Early Visean time (crystalline basement of the craton, eroded Meso-and Neoproterozoic sedimentary complexes, and igneous rocks of Central Taimyr) contributed significantly to the accumulation of the Late Visean-Serpukhovian deposits. In the rocks of the Tiksi Formation, 45% of detrital zircons are of Paleozoic age, while 24% are Early Paleozoic, with prevailing Cambrian a

AB - The first U-Pb dating of detrital zircons from the Lower Carboniferous sandstones in the frontal part of the northern Verkhoyansk fold-and-thrust belt showed that detrital zircon age spectra for the Lower Visean (Krestyakh Formation) and the Upper Visean-Serpukhovian (Tiksi Formation) rocks are quite different. The Early Visean sandstones contain up to 95% detrital zircons of Precambrian age, while those of Late Visean-Serpukhovian age, only 55%. The shape of age distribution plots of Precambrian zircons for both samples is similar, indicating that reworking of terrigenous sediments of the Krestyakh Formation or the same sources dominated in Early Visean time (crystalline basement of the craton, eroded Meso-and Neoproterozoic sedimentary complexes, and igneous rocks of Central Taimyr) contributed significantly to the accumulation of the Late Visean-Serpukhovian deposits. In the rocks of the Tiksi Formation, 45% of detrital zircons are of Paleozoic age, while 24% are Early Paleozoic, with prevailing Cambrian a

U2 - 10.1016/j.rgg.2013.09.005

DO - 10.1016/j.rgg.2013.09.005

M3 - Article

SP - 1195

EP - 1204

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 10

ER -

ID: 5674961