Large paleoearthquakes and Holocene faulting in the Southeastern Gorny Altai: implications for ongoing crustal shortening in Central Asia

Author:

Deev Evgeny V.12,Panin Andrey V.3,Solomina Olga N.3,Bricheva Svetlana S.134,Borodovskiy Andrey P.56,Entin Andrey L.7,Kurbanov Redzhep N.37

Affiliation:

1. Department of Geology and Geophysics, Novosibirsk State University, Novosibirsk, Russia

2. A.A. Trofimuk Institute of Petroleum Geology and Geophysics, Russian Academy of Sciences, Siberian Branch, Novosibirsk, Russia

3. Institute of Geography, Russian Academy of Sciences, Moscow, Russia

4. Department of Geology, Lomonosov Moscow State University, Moscow, Russia

5. Institute of Archaeology and Ethnography, Siberian Branch of the Russian Academy of Sciences, Novosibirsk, Russia

6. Department of History and Political Studies, Tomsk State University, Tomsk, Russia

7. Department of Geography, Lomonosov Moscow State University, Moscow, Russia

Funder

Russian Science Foundation

Publisher

Informa UK Limited

Reference58 articles.

1. Annan, A.P., 2003, Ground penetrating radar principles, procedures & applications: Sensors & Software Inc. 286P.

2. THE ACTIVE FAULTS OF EURASIA DATABASE

3. `Forebergs', flower structures, and the development of large intra-continental strike-slip faults: the Gurvan Bogd fault system in Mongolia

4. Bondarenko, P.M., Devyatkin, E.V., and Liskun, I.G., 1968, Cenozoic neotectonics and stratigraphy of the Aktash region in the kurai neotectonic zone of Gorny Altai. In: Problems of Geomorphology and Neotectonics of Mountain Provinces in Siberia and Russian Far East Proceedings USSR Workshop on Geomorphology and Neotectonics of Siberia and Russian Far East: Nauka, Novosibirsk, Book II, p. 65–73. (in Russian).

5. Numerical simulation of ground‐penetrating radar data for studying the geometry of fault zone

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