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The Paleomagnetic Pole of the Siberian Paleocontinent at the Late Ediacaran Stage of Evolution of the Active Continental Margin (South Yenisei Ridge). / Kadilnikov, P. I.; Vernikovskaya, A. E.; Mikhaltsov, N. E. и др.

в: Doklady Earth Sciences, Том 483, № 1, 01.12.2018, стр. 1394-1398.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Kadilnikov, PI, Vernikovskaya, AE, Mikhaltsov, NE, Vernikovsky, VA & Matushkin, NY 2018, 'The Paleomagnetic Pole of the Siberian Paleocontinent at the Late Ediacaran Stage of Evolution of the Active Continental Margin (South Yenisei Ridge)', Doklady Earth Sciences, Том. 483, № 1, стр. 1394-1398. https://doi.org/10.1134/S1028334X18110089

APA

Kadilnikov, P. I., Vernikovskaya, A. E., Mikhaltsov, N. E., Vernikovsky, V. A., & Matushkin, N. Y. (2018). The Paleomagnetic Pole of the Siberian Paleocontinent at the Late Ediacaran Stage of Evolution of the Active Continental Margin (South Yenisei Ridge). Doklady Earth Sciences, 483(1), 1394-1398. https://doi.org/10.1134/S1028334X18110089

Vancouver

Kadilnikov PI, Vernikovskaya AE, Mikhaltsov NE, Vernikovsky VA, Matushkin NY. The Paleomagnetic Pole of the Siberian Paleocontinent at the Late Ediacaran Stage of Evolution of the Active Continental Margin (South Yenisei Ridge). Doklady Earth Sciences. 2018 дек. 1;483(1):1394-1398. doi: 10.1134/S1028334X18110089

Author

Kadilnikov, P. I. ; Vernikovskaya, A. E. ; Mikhaltsov, N. E. и др. / The Paleomagnetic Pole of the Siberian Paleocontinent at the Late Ediacaran Stage of Evolution of the Active Continental Margin (South Yenisei Ridge). в: Doklady Earth Sciences. 2018 ; Том 483, № 1. стр. 1394-1398.

BibTeX

@article{37664d16be95461bb34d6563fe129366,
title = "The Paleomagnetic Pole of the Siberian Paleocontinent at the Late Ediacaran Stage of Evolution of the Active Continental Margin (South Yenisei Ridge)",
abstract = "Abstract: The results of the first paleomagnetic study of a late Neoproterozoic magmatic complex on the Siberian paleocontinent (Siberia) using U–Pb geochronological data are presented. The igneous rocks of the Zimoveyniy massif (block) of the South Yenisei Ridge formed in an active continental margin setting and recorded the initial thermoremanent magnetization. Our calculations let us determine with reasonable certitude that in the late Ediacaran Siberia was located in the subequatorial latitudes.",
keywords = "MAGMATISM, CRATON",
author = "Kadilnikov, {P. I.} and Vernikovskaya, {A. E.} and Mikhaltsov, {N. E.} and Vernikovsky, {V. A.} and Matushkin, {N. Yu}",
year = "2018",
month = dec,
day = "1",
doi = "10.1134/S1028334X18110089",
language = "English",
volume = "483",
pages = "1394--1398",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - The Paleomagnetic Pole of the Siberian Paleocontinent at the Late Ediacaran Stage of Evolution of the Active Continental Margin (South Yenisei Ridge)

AU - Kadilnikov, P. I.

AU - Vernikovskaya, A. E.

AU - Mikhaltsov, N. E.

AU - Vernikovsky, V. A.

AU - Matushkin, N. Yu

PY - 2018/12/1

Y1 - 2018/12/1

N2 - Abstract: The results of the first paleomagnetic study of a late Neoproterozoic magmatic complex on the Siberian paleocontinent (Siberia) using U–Pb geochronological data are presented. The igneous rocks of the Zimoveyniy massif (block) of the South Yenisei Ridge formed in an active continental margin setting and recorded the initial thermoremanent magnetization. Our calculations let us determine with reasonable certitude that in the late Ediacaran Siberia was located in the subequatorial latitudes.

AB - Abstract: The results of the first paleomagnetic study of a late Neoproterozoic magmatic complex on the Siberian paleocontinent (Siberia) using U–Pb geochronological data are presented. The igneous rocks of the Zimoveyniy massif (block) of the South Yenisei Ridge formed in an active continental margin setting and recorded the initial thermoremanent magnetization. Our calculations let us determine with reasonable certitude that in the late Ediacaran Siberia was located in the subequatorial latitudes.

KW - MAGMATISM

KW - CRATON

UR - http://www.scopus.com/inward/record.url?scp=85058864348&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18110089

DO - 10.1134/S1028334X18110089

M3 - Article

AN - SCOPUS:85058864348

VL - 483

SP - 1394

EP - 1398

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 17927550