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


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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.

About the authors

V. V. Ruzhich

Institute of the Earth’s Crust, Siberian Branch

Email: gevorgkidg@mail.ru
Russian Federation, Irkutsk, 664033

G. G. Kocharyan

Institute of Geosphere Dynamics

Author for correspondence.
Email: gevorgkidg@mail.ru
Russian Federation, Moscow, 119334

A. V. Travin

Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk State University

Email: gevorgkidg@mail.ru
Russian Federation, Novosibirsk, 630090; Novosibirsk, 630090

V. B. Savel’eva

Institute of the Earth’s Crust, Siberian Branch

Email: gevorgkidg@mail.ru
Russian Federation, Irkutsk, 664033

A. A. Ostapchuk

Institute of Geosphere Dynamics

Email: gevorgkidg@mail.ru
Russian Federation, Moscow, 119334

S. V. Rasskazov

Institute of the Earth’s Crust, Siberian Branch; Irkutsk State University

Email: gevorgkidg@mail.ru
Russian Federation, Irkutsk, 664033; Irkutsk, 664003

T. A. Yasnygina

Institute of the Earth’s Crust, Siberian Branch

Email: gevorgkidg@mail.ru
Russian Federation, Irkutsk, 664033

D. S. Yudin

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: gevorgkidg@mail.ru
Russian Federation, Novosibirsk, 630090

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