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

V. V. Ruzhich; G. G. Kocharyan; A. V. Travin; V. B. Savel’eva; A. A. Ostapchuk; S. V. Rasskazov; T. A. Yasnygina; D. S. Yudin

doi:10.1134/S1028334X18080081

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

Autores: Ruzhich V.V.¹, Kocharyan G.G.², Travin A.V.³^,4, Savel’eva V.B.¹, Ostapchuk A.A.², Rasskazov S.V.¹^,5, Yasnygina T.A.¹, Yudin D.S.³
Afiliações:
1. Institute of the Earth’s Crust, Siberian Branch
2. Institute of Geosphere Dynamics
3. Sobolev Institute of Geology and Mineralogy, Siberian Branch
4. Novosibirsk State University
5. Irkutsk State University
Edição: Volume 481, Nº 2 (2018)
Páginas: 1017-1020
Seção: Geophysics
URL: https://bakhtiniada.ru/1028-334X/article/view/193809
DOI: https://doi.org/10.1134/S1028334X18080081
ID: 193809

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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.