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Determination of the PT Conditions that Accompanied a Seismogenic Slip along a Deep Segment of the Marginal Suture of the Siberian Craton. / Ruzhich, V. V.; Kocharyan, G. G.; Travin, A. V. и др.

в: Doklady Earth Sciences, Том 481, № 2, 01.08.2018, стр. 1017-1020.

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

Harvard

Ruzhich, VV, Kocharyan, GG, Travin, AV, Savel’eva, VB, Ostapchuk, AA, Rasskazov, SV, Yasnygina, TA & Yudin, DS 2018, 'Determination of the PT Conditions that Accompanied a Seismogenic Slip along a Deep Segment of the Marginal Suture of the Siberian Craton', Doklady Earth Sciences, Том. 481, № 2, стр. 1017-1020. https://doi.org/10.1134/S1028334X18080081

APA

Ruzhich, V. V., Kocharyan, G. G., Travin, A. V., Savel’eva, V. B., Ostapchuk, A. A., Rasskazov, S. V., Yasnygina, T. A., & Yudin, D. S. (2018). Determination of the PT Conditions that Accompanied a Seismogenic Slip along a Deep Segment of the Marginal Suture of the Siberian Craton. Doklady Earth Sciences, 481(2), 1017-1020. https://doi.org/10.1134/S1028334X18080081

Vancouver

Ruzhich VV, Kocharyan GG, Travin AV, Savel’eva VB, Ostapchuk AA, Rasskazov SV и др. Determination of the PT Conditions that Accompanied a Seismogenic Slip along a Deep Segment of the Marginal Suture of the Siberian Craton. Doklady Earth Sciences. 2018 авг. 1;481(2):1017-1020. doi: 10.1134/S1028334X18080081

Author

Ruzhich, V. V. ; Kocharyan, G. G. ; Travin, A. V. и др. / Determination of the PT Conditions that Accompanied a Seismogenic Slip along a Deep Segment of the Marginal Suture of the Siberian Craton. в: Doklady Earth Sciences. 2018 ; Том 481, № 2. стр. 1017-1020.

BibTeX

@article{486784503b9946da803f45178cc95ac1,
title = "Determination of the PT Conditions that Accompanied a Seismogenic Slip along a Deep Segment of the Marginal Suture of the Siberian Craton",
abstract = "This paper reports data on the structure of the central zone of the seismogenic fault in the originally deep segments of the fault zone. The isotopic analyses have made it possible to estimate the absolute age of the ancient coseismic faults at 673 ± 5 Ma, which is indicative of seismic activation of deep faults in the studied segment of the marginal suture of the Siberian Craton in the Neoproterozoic.",
author = "Ruzhich, {V. V.} and Kocharyan, {G. G.} and Travin, {A. V.} and Savel{\textquoteright}eva, {V. B.} and Ostapchuk, {A. A.} and Rasskazov, {S. V.} and Yasnygina, {T. A.} and Yudin, {D. S.}",
note = "Publisher Copyright: {\textcopyright} 2018, Pleiades Publishing, Ltd.",
year = "2018",
month = aug,
day = "1",
doi = "10.1134/S1028334X18080081",
language = "English",
volume = "481",
pages = "1017--1020",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Determination of the PT Conditions that Accompanied a Seismogenic Slip along a Deep Segment of the Marginal Suture of the Siberian Craton

AU - Ruzhich, V. V.

AU - Kocharyan, G. G.

AU - Travin, A. V.

AU - Savel’eva, V. B.

AU - Ostapchuk, A. A.

AU - Rasskazov, S. V.

AU - Yasnygina, T. A.

AU - Yudin, D. S.

N1 - Publisher Copyright: © 2018, Pleiades Publishing, Ltd.

PY - 2018/8/1

Y1 - 2018/8/1

N2 - This paper reports data on the structure of the central zone of the seismogenic fault in the originally deep segments of the fault zone. The isotopic analyses have made it possible to estimate the absolute age of the ancient coseismic faults at 673 ± 5 Ma, which is indicative of seismic activation of deep faults in the studied segment of the marginal suture of the Siberian Craton in the Neoproterozoic.

AB - This paper reports data on the structure of the central zone of the seismogenic fault in the originally deep segments of the fault zone. The isotopic analyses have made it possible to estimate the absolute age of the ancient coseismic faults at 673 ± 5 Ma, which is indicative of seismic activation of deep faults in the studied segment of the marginal suture of the Siberian Craton in the Neoproterozoic.

UR - http://www.scopus.com/inward/record.url?scp=85052840755&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18080081

DO - 10.1134/S1028334X18080081

M3 - Article

AN - SCOPUS:85052840755

VL - 481

SP - 1017

EP - 1020

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 16358149