The Zagan earthquake of February 1, 2011, in the low-seismoactive zone of western Transbaikalia: Observations and analysis


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We described the February 1, 2011 (Mw = 4.7) Zagan earthquake occurred in the area of the Zagan range. This event is one of the most significant in western Transbaikalia. Macroseismic effects of this seismic event were felt over a wide territory: the intensity of II was observed at the distance of more than 300 km. Earthquake focal parameters (hypocentral depth, seismic moment, moment magnitude and focal mechanism) calculated from the data on surface wave amplitude spectra correspond to the structural position of the origin connected with a zone of plastic flow (slip) bordering the northwest slope of the Zagan range (similar complex of the metamorphic core). The results obtained prove the existence of the continental extension processes in this area.

作者简介

V. Melnikova

Institute of the Earth’s Crust

编辑信件的主要联系方式.
Email: vimel@crust.irk.ru
俄罗斯联邦, ul. Lermontova 128, Irkutsk, 664033

A. Seredkina

Institute of the Earth’s Crust

Email: vimel@crust.irk.ru
俄罗斯联邦, ul. Lermontova 128, Irkutsk, 664033

Ya. Radziminovich

Institute of the Earth’s Crust

Email: vimel@crust.irk.ru
俄罗斯联邦, ul. Lermontova 128, Irkutsk, 664033

A. Melnikov

Institute of the Earth’s Crust

Email: vimel@crust.irk.ru
俄罗斯联邦, ul. Lermontova 128, Irkutsk, 664033

N. Gilyova

Baikalian Branch of the Geophysical Survey

Email: vimel@crust.irk.ru
俄罗斯联邦, ul. Lermontova 128, Irkutsk, 664033

Ts. Tubanov

Institute of Geology

Email: vimel@crust.irk.ru
俄罗斯联邦, ul. Sakh’yanovoi 6a, Ulan-Ude, Republic of Buryatia, 670047


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