Standard

Trans-Siberian Permian rivers: A key to understanding Arctic sedimentary provenance. / Ershova, V.B.; Khudoley, A.K.; Prokopiev, A.V.; Tuchkova, M.I.; Fedorov, P.V.; Kazakova, G.G.; Shishlov, S.B.; O'Sullivan, P.

In: Tectonophysics, Vol. 691, No. 220-233, 2016, p. 220-233.

Research output: Contribution to journal › Article

Harvard

Ershova, VB, Khudoley, AK, Prokopiev, AV, Tuchkova, MI, Fedorov, PV, Kazakova, GG, Shishlov, SB & O'Sullivan, P 2016, 'Trans-Siberian Permian rivers: A key to understanding Arctic sedimentary provenance', Tectonophysics, vol. 691, no. 220-233, pp. 220-233. https://doi.org/10.1016/j.tecto.2016.03.028

APA

Ershova, V. B., Khudoley, A. K., Prokopiev, A. V., Tuchkova, M. I., Fedorov, P. V., Kazakova, G. G., Shishlov, S. B., & O'Sullivan, P. (2016). Trans-Siberian Permian rivers: A key to understanding Arctic sedimentary provenance. Tectonophysics, 691(220-233), 220-233. https://doi.org/10.1016/j.tecto.2016.03.028

Vancouver

Ershova VB, Khudoley AK, Prokopiev AV, Tuchkova MI, Fedorov PV, Kazakova GG et al. Trans-Siberian Permian rivers: A key to understanding Arctic sedimentary provenance. Tectonophysics. 2016;691(220-233):220-233. https://doi.org/10.1016/j.tecto.2016.03.028

Author

Ershova, V.B. ; Khudoley, A.K. ; Prokopiev, A.V. ; Tuchkova, M.I. ; Fedorov, P.V. ; Kazakova, G.G. ; Shishlov, S.B. ; O'Sullivan, P. / Trans-Siberian Permian rivers: A key to understanding Arctic sedimentary provenance. In: Tectonophysics. 2016 ; Vol. 691, No. 220-233. pp. 220-233.

BibTeX

@article{a23ca4bb6406451a985b7368526f8343,
title = "Trans-Siberian Permian rivers: A key to understanding Arctic sedimentary provenance",
abstract = "{\textcopyright} 2016 Elsevier B.V.Permian strata of northern Siberia contain a rich record of the late Paleozoic history of Siberia and surrounding fold and thrust belts (FTB). More than 850 uranium-lead (U-Pb) detrital zircon ages collected from the Permian strata provide vital information about sediment source areas and history of the sedimentary basins. The detrital zircon populations obtained from the Permian clastics of northern Siberia are characterized by large percentages of late Paleozoic and early Paleozoic zircons, whose ages can be correlated with magmatic events known from the Ural-Mongolian Orogen. Our data suggest that Permian clastics of northern Siberia were mainly sourced from orogens developed along the western and southwestern margins of the Siberian Craton (in present-day coordinates), with an additional sediment contribution from the reworked sedimentary cover and basement of Siberia. The contribution from Siberian sources is distinguished in the Precambrian part of the detrital zircon populations by",
author = "V.B. Ershova and A.K. Khudoley and A.V. Prokopiev and M.I. Tuchkova and P.V. Fedorov and G.G. Kazakova and S.B. Shishlov and P. O'Sullivan",
year = "2016",
doi = "10.1016/j.tecto.2016.03.028",
language = "English",
volume = "691",
pages = "220--233",
journal = "Tectonophysics",
issn = "0040-1951",
publisher = "Elsevier",
number = "220-233",

}

RIS

TY - JOUR

T1 - Trans-Siberian Permian rivers: A key to understanding Arctic sedimentary provenance

AU - Ershova, V.B.

AU - Khudoley, A.K.

AU - Prokopiev, A.V.

AU - Tuchkova, M.I.

AU - Fedorov, P.V.

AU - Kazakova, G.G.

AU - Shishlov, S.B.

AU - O'Sullivan, P.

PY - 2016

Y1 - 2016

N2 - © 2016 Elsevier B.V.Permian strata of northern Siberia contain a rich record of the late Paleozoic history of Siberia and surrounding fold and thrust belts (FTB). More than 850 uranium-lead (U-Pb) detrital zircon ages collected from the Permian strata provide vital information about sediment source areas and history of the sedimentary basins. The detrital zircon populations obtained from the Permian clastics of northern Siberia are characterized by large percentages of late Paleozoic and early Paleozoic zircons, whose ages can be correlated with magmatic events known from the Ural-Mongolian Orogen. Our data suggest that Permian clastics of northern Siberia were mainly sourced from orogens developed along the western and southwestern margins of the Siberian Craton (in present-day coordinates), with an additional sediment contribution from the reworked sedimentary cover and basement of Siberia. The contribution from Siberian sources is distinguished in the Precambrian part of the detrital zircon populations by

AB - © 2016 Elsevier B.V.Permian strata of northern Siberia contain a rich record of the late Paleozoic history of Siberia and surrounding fold and thrust belts (FTB). More than 850 uranium-lead (U-Pb) detrital zircon ages collected from the Permian strata provide vital information about sediment source areas and history of the sedimentary basins. The detrital zircon populations obtained from the Permian clastics of northern Siberia are characterized by large percentages of late Paleozoic and early Paleozoic zircons, whose ages can be correlated with magmatic events known from the Ural-Mongolian Orogen. Our data suggest that Permian clastics of northern Siberia were mainly sourced from orogens developed along the western and southwestern margins of the Siberian Craton (in present-day coordinates), with an additional sediment contribution from the reworked sedimentary cover and basement of Siberia. The contribution from Siberian sources is distinguished in the Precambrian part of the detrital zircon populations by

U2 - 10.1016/j.tecto.2016.03.028

DO - 10.1016/j.tecto.2016.03.028

M3 - Article

VL - 691

SP - 220

EP - 233

JO - Tectonophysics

JF - Tectonophysics

SN - 0040-1951

IS - 220-233

ER -

ID: 4003059