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Results of U–Pb (LA–ICPMS) dating of detrital zircons from metaterrigenous rocks of the basement of the North Kara basin. / Ershova, V.B.; Prokopiev, A.V.; Khudoley, A.K.; Shneider, G.V.; Andersen, T.; Kullerud, K.; Makar’ev, A.A.; Maslov, A.V.; Kolchanov, D.A.

In: Doklady Earth Sciences, No. 2, 2015, p. 997-1000.

Research output: Contribution to journal › Article

Harvard

Ershova, VB, Prokopiev, AV, Khudoley, AK, Shneider, GV, Andersen, T, Kullerud, K, Makar’ev, AA, Maslov, AV & Kolchanov, DA 2015, 'Results of U–Pb (LA–ICPMS) dating of detrital zircons from metaterrigenous rocks of the basement of the North Kara basin', Doklady Earth Sciences, no. 2, pp. 997-1000. https://doi.org/10.1134/S1028334X15100013

APA

Ershova, V. B., Prokopiev, A. V., Khudoley, A. K., Shneider, G. V., Andersen, T., Kullerud, K., Makar’ev, A. A., Maslov, A. V., & Kolchanov, D. A. (2015). Results of U–Pb (LA–ICPMS) dating of detrital zircons from metaterrigenous rocks of the basement of the North Kara basin. Doklady Earth Sciences, (2), 997-1000. https://doi.org/10.1134/S1028334X15100013

Vancouver

Ershova VB, Prokopiev AV, Khudoley AK, Shneider GV, Andersen T, Kullerud K et al. Results of U–Pb (LA–ICPMS) dating of detrital zircons from metaterrigenous rocks of the basement of the North Kara basin. Doklady Earth Sciences. 2015;(2):997-1000. https://doi.org/10.1134/S1028334X15100013

Author

Ershova, V.B. ; Prokopiev, A.V. ; Khudoley, A.K. ; Shneider, G.V. ; Andersen, T. ; Kullerud, K. ; Makar’ev, A.A. ; Maslov, A.V. ; Kolchanov, D.A. / Results of U–Pb (LA–ICPMS) dating of detrital zircons from metaterrigenous rocks of the basement of the North Kara basin. In: Doklady Earth Sciences. 2015 ; No. 2. pp. 997-1000.

BibTeX

@article{fe13ad3f0c7241cb933363b54add99eb,
title = "Results of U–Pb (LA–ICPMS) dating of detrital zircons from metaterrigenous rocks of the basement of the North Kara basin",
abstract = "{\textcopyright} 2015, Pleiades Publishing, Ltd.The U–Pb (LA–ICPMS) age was established for detrital zircons from the oldest, intensely deformed metasedimentary complexes without reliable fossils{\textquoteright} record, which represent the folded basement of the North Kara basin and are exposed on Bol{\textquoteright}shevik and Troinoi islands (Severnaya Zemlya and Izvestii TSIK archipelagoes, respectively). Our data suggest the common evolution of the Cambrian–Ordovician sequences exposed on the islands of both archipelagoes.",
author = "V.B. Ershova and A.V. Prokopiev and A.K. Khudoley and G.V. Shneider and T. Andersen and K. Kullerud and A.A. Makar{\textquoteright}ev and A.V. Maslov and D.A. Kolchanov",
year = "2015",
doi = "10.1134/S1028334X15100013",
language = "English",
pages = "997--1000",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - Results of U–Pb (LA–ICPMS) dating of detrital zircons from metaterrigenous rocks of the basement of the North Kara basin

AU - Ershova, V.B.

AU - Prokopiev, A.V.

AU - Khudoley, A.K.

AU - Shneider, G.V.

AU - Andersen, T.

AU - Kullerud, K.

AU - Makar’ev, A.A.

AU - Maslov, A.V.

AU - Kolchanov, D.A.

PY - 2015

Y1 - 2015

N2 - © 2015, Pleiades Publishing, Ltd.The U–Pb (LA–ICPMS) age was established for detrital zircons from the oldest, intensely deformed metasedimentary complexes without reliable fossils’ record, which represent the folded basement of the North Kara basin and are exposed on Bol’shevik and Troinoi islands (Severnaya Zemlya and Izvestii TSIK archipelagoes, respectively). Our data suggest the common evolution of the Cambrian–Ordovician sequences exposed on the islands of both archipelagoes.

AB - © 2015, Pleiades Publishing, Ltd.The U–Pb (LA–ICPMS) age was established for detrital zircons from the oldest, intensely deformed metasedimentary complexes without reliable fossils’ record, which represent the folded basement of the North Kara basin and are exposed on Bol’shevik and Troinoi islands (Severnaya Zemlya and Izvestii TSIK archipelagoes, respectively). Our data suggest the common evolution of the Cambrian–Ordovician sequences exposed on the islands of both archipelagoes.

U2 - 10.1134/S1028334X15100013

DO - 10.1134/S1028334X15100013

M3 - Article

SP - 997

EP - 1000

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 4003003