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Integrated provenance analysis of Carboniferous deposits from Northeastern Siberia: Implication for the late Paleozoic history of the Arctic. / Ershova, V.B.; Prokopiev, A.V.; Khudoley, A.K.

в: Journal of Asian Earth Sciences, Том 109, № 2, 2015, стр. 38-49.

Результаты исследований: Научные публикации в периодических изданиях › статья

Harvard

Ershova, VB, Prokopiev, AV & Khudoley, AK 2015, 'Integrated provenance analysis of Carboniferous deposits from Northeastern Siberia: Implication for the late Paleozoic history of the Arctic', Journal of Asian Earth Sciences, Том. 109, № 2, стр. 38-49. https://doi.org/10.1016/j.jseaes.2015.04.046

APA

Ershova, V. B., Prokopiev, A. V., & Khudoley, A. K. (2015). Integrated provenance analysis of Carboniferous deposits from Northeastern Siberia: Implication for the late Paleozoic history of the Arctic. Journal of Asian Earth Sciences, 109(2), 38-49. https://doi.org/10.1016/j.jseaes.2015.04.046

Vancouver

Ershova VB, Prokopiev AV, Khudoley AK. Integrated provenance analysis of Carboniferous deposits from Northeastern Siberia: Implication for the late Paleozoic history of the Arctic. Journal of Asian Earth Sciences. 2015;109(2):38-49. https://doi.org/10.1016/j.jseaes.2015.04.046

Author

Ershova, V.B. ; Prokopiev, A.V. ; Khudoley, A.K. / Integrated provenance analysis of Carboniferous deposits from Northeastern Siberia: Implication for the late Paleozoic history of the Arctic. в: Journal of Asian Earth Sciences. 2015 ; Том 109, № 2. стр. 38-49.

BibTeX

@article{14e4814e30cb49839e35fe09c6bd14d1,
title = "Integrated provenance analysis of Carboniferous deposits from Northeastern Siberia: Implication for the late Paleozoic history of the Arctic",
abstract = "{\textcopyright} 2015 Elsevier Ltd. An integrated provenance analysis based on sandstone petrography, distribution of REE and trace elements, and U/Pb detrital zircon dating of Carboniferous sedimentary rocks of northern Verkhoyansk Fold and Thrust Belt (FTB) provides new insights into the tectonic evolution of NE Siberia. According to petrographic and geochemical data, Lower Visean sandstones had local provenance that contained mafic magmatic rocks. Wide distribution of ca. 2075. Ma detrital zircons known in the basement of neighboring Olenek and Ust'-Lena uplifts supports local provenance of the Lower Visean sandstones. Starting from Late Visean, clastic sediments have geochemical and petrographic compositions that are characteristic for erosion predominantly felsic rocks in a more remote source region. Detrital zircon age distributions in the Upper Visean - Upper Carboniferous sandstones, point to Taymyr - Severnaya Zemlya FTB and Central Asian Orogenic Belt (CAOB) as the most likely provenances for clastic rocks. Howeve",
author = "V.B. Ershova and A.V. Prokopiev and A.K. Khudoley",
year = "2015",
doi = "10.1016/j.jseaes.2015.04.046",
language = "English",
volume = "109",
pages = "38--49",
journal = "Journal of Asian Earth Sciences",
issn = "1367-9120",
publisher = "Elsevier",
number = "2",

}

RIS

TY - JOUR

T1 - Integrated provenance analysis of Carboniferous deposits from Northeastern Siberia: Implication for the late Paleozoic history of the Arctic

AU - Ershova, V.B.

AU - Prokopiev, A.V.

AU - Khudoley, A.K.

PY - 2015

Y1 - 2015

N2 - © 2015 Elsevier Ltd. An integrated provenance analysis based on sandstone petrography, distribution of REE and trace elements, and U/Pb detrital zircon dating of Carboniferous sedimentary rocks of northern Verkhoyansk Fold and Thrust Belt (FTB) provides new insights into the tectonic evolution of NE Siberia. According to petrographic and geochemical data, Lower Visean sandstones had local provenance that contained mafic magmatic rocks. Wide distribution of ca. 2075. Ma detrital zircons known in the basement of neighboring Olenek and Ust'-Lena uplifts supports local provenance of the Lower Visean sandstones. Starting from Late Visean, clastic sediments have geochemical and petrographic compositions that are characteristic for erosion predominantly felsic rocks in a more remote source region. Detrital zircon age distributions in the Upper Visean - Upper Carboniferous sandstones, point to Taymyr - Severnaya Zemlya FTB and Central Asian Orogenic Belt (CAOB) as the most likely provenances for clastic rocks. Howeve

AB - © 2015 Elsevier Ltd. An integrated provenance analysis based on sandstone petrography, distribution of REE and trace elements, and U/Pb detrital zircon dating of Carboniferous sedimentary rocks of northern Verkhoyansk Fold and Thrust Belt (FTB) provides new insights into the tectonic evolution of NE Siberia. According to petrographic and geochemical data, Lower Visean sandstones had local provenance that contained mafic magmatic rocks. Wide distribution of ca. 2075. Ma detrital zircons known in the basement of neighboring Olenek and Ust'-Lena uplifts supports local provenance of the Lower Visean sandstones. Starting from Late Visean, clastic sediments have geochemical and petrographic compositions that are characteristic for erosion predominantly felsic rocks in a more remote source region. Detrital zircon age distributions in the Upper Visean - Upper Carboniferous sandstones, point to Taymyr - Severnaya Zemlya FTB and Central Asian Orogenic Belt (CAOB) as the most likely provenances for clastic rocks. Howeve

U2 - 10.1016/j.jseaes.2015.04.046

DO - 10.1016/j.jseaes.2015.04.046

M3 - Article

VL - 109

SP - 38

EP - 49

JO - Journal of Asian Earth Sciences

JF - Journal of Asian Earth Sciences

SN - 1367-9120

IS - 2

ER -

ID: 3946607