I. V. Turova

Institute of Petroleum Geology and Geophysics

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E. V. Deev

Novosibirsk State University

АВ

А. В. Панин

Institute of Geography

АМ

А. М. Корженков

Schmidt Institute of Physics of the Earth

ЕА

Е. А. Рогожин

Schmidt Institute of Physics of the Earth

A. B. Fortuna

National Academy of Sciences of the Republic of Kyrgyzstan

M. A. Bronnikova

Institute of Geography

S. V. Abdieva

Kyrgyz-Russian Slavic University named after B.N. Yeltsin

I. D. Zolnikov

Russian Academy of Sciences

Jonas Mažeika

Nature Research Centre

Andrey L. Entin

Lomonosov Moscow State University

Cooperative Institutions

Russian Academy of Sciences

Institute of Geography

V. B. Sochava Institute of Geography

Lomonosov Moscow State University

Moscow State University

Novosibirsk State University

Siberian Branch of the Russian Academy of Sciences

Kyrgyz-Russian Slavic University named after B.N. Yeltsin

Schmidt Institute of Physics of the Earth

Institute of the Earth’s Crust

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Record of Holocene Changes in High-Mountain Landscapes of Southeastern Altai in the Soil–Sedimentary Sequence of the Boguty River Valley

Eurasian Soil Science (2018)

M. A. Bronnikova А. Р. Агатова М. П. Лебедева Р. К. Непоп Yu. V. Konoplianikova

Steppe

Paleosol

Humus

Solifluction

Pedology

10.1134/s1064229318120037

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Citations (10)

Properties of ancient deeply transformed man-made soils (cultural layers) and their advances to classification by the example of Early Iron Age sites in Moscow Region

CATENA (2014)

Alexandra Golyeva Э. П. Зазовская I. V. Turova

Human settlement

Iron Age

10.1016/j.catena.2014.12.030

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Citations (21)

Paleoearthquakes in the Uimon basin (Gorny Altai)

Russian Geology and Geophysics (2018)

E. V. Deev I. D. Zolnikov I. V. Turova G.G. Rusanov Yu. M. Ryapolova

Rockslide

Paleoseismology

Alluvial fan

10.1016/j.rgg.2017.07.011

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Citations (12)

Paleoseismicity along Adyr faults (on example of Kokonadyr-Tegerek fault in South-Western Issyk-Kul lake region, Tien Shan)

Вулканология и сейсмология (2019)

А. М. Корженков S. V. Abdieva A. S. Gladkov E. V. Deev Ts. Liu

We have studied paleoseismicity along a zone of the Kokonadyr-Tegerek adyr (foothill) fault in SW Issyk-Kul Lake region. It was shown that, although seismic movements continue along a zone of the tectonic contact of Paleozoic rocks of the Kokonadyr-Tegerek uplift and Quaternary deposits of the Alabash-Konurolyong depression, main number of appearance of seismogenic ruptures in the surface shift southward on hundreds of meters from the adyr fault mentioned above. This process leads to a formation of multiple fault scarps and compensation grabens in their back parts. According to data of radiocarbon dating along the Kokonadyr-Tegerek fault zone there were 4 strong Holocene earthquakes occurred during time intervals: 1771–1785 AD, 1440–1515 AD, and also possibly in 2310–745 BC and 640–5300 BC. Judging by parameters of the fault scarps their magnitudes were M ≥ 7, and seismic intensity I0≥ IX. Strong seismic activity along the Kokonadyr-Tegerek fault zone continues at least from Mid-Pleistocene. Evidences of this statement are uplifted and abandoned river valley of that time in the uplift with the same name as well as significant accumulation of the lacustrine sediments in northern part of the Alabash-Konurolyong depression. Large thickness of the sediments is tied with glaciers melting in the northern slope of the Terskey Ala-Too Range, and abandoned valleys testify on significant tectonic damming. Most proper model explaining formation of the adyrs (foothills) in the southern part of the Issyk-Kul Depression is a model of a gently dipping main fault flattening out northward, which is complicated by the underthrusts. All obtained data can be used at compilation of a new Map of Seismic Hazard of Kyrgyz Republic.

10.31857/s0203-03062019536-53

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Citations (1)

Cryo-geomorphological evolution of soils on islands of Terekhol Lake, Tyva, Southern Siberia

Eurasian Soil Science (2010)

M. A. Bronnikova А. В. Панин I. V. Turova O. N. Uspenskaya Е. П. Кузнецова

Paleosol

10.1134/s1064229310130090

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Citations (3)

Results of paleoseismological studies along the planned route of the gas pipeline to the people’s republic of China (Kurai fault zone, Gorny Altai)

Материалы XVI Всероссийской научно-технической конференции студентов и аспирантов : посвящается 90-летию Уральского государственного лесотехнического университета (УЛТИ УГЛТА УГЛТУ) (2020)

I. V. Turova E. V. Deev N. I. Pozdnyakova Andrey L. Entin Н. Н. Неведрова

The Kurai Fault Zone have generated paleoearthquakes with Mw = 6.6–7.6 and ESI 2007 shaking intensities of VIII to XI. The paleoearthquakes occurred ca. 6.3, 5.8, 3.2, and 1.3 ka BP, in the second half of the 18th centuries AD. ERT and GPR data reveals the resistivity structure of the area with seismogenic faults traceable to depths of 40–50 m. The conclusions above must be taken into account when design and constructing the gas pipeline from Russia to the People’s Republic of China.

Gas Pipeline

People's Republic

10.18303/b978-5-4262-0102-6-2020-070

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Citations (0)

Paleoseismological and archaeoseismological data from the western Alabash–Konurolen intramontane basin (southern Lake Issyk Kul area, Kyrgyzstan)

Russian Geology and Geophysics (2016)

E. V. Deev I. V. Turova А. М. Корженков D.V. Luzhansky А. С. Гладков

Paleoseismology

10.1016/j.rgg.2016.06.008

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Citations (16)

Large ancient earthquakes in the western Issyk-Kul basin (Kyrgyzstan, northern Tien Shan)

Journal of Asian Earth Sciences (2018)

E. V. Deev Andrey Korzhenkov I. V. Turova Terry L. Pavlis D. V. Luzhanskii

Paleoseismology

Thrust fault

Basement

10.1016/j.jseaes.2018.07.019

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Citations (16)

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

Near Surface Geophysics (2021)

С. С. Бричева Ivan Dubrovin О. В. Лунина I. A. Denisenko Victor Matasov

ABSTRACT Palaeoseismology studies the footprints of ancient earthquakes to improve the knowledge about the modern seismicity of the territory. A ground‐penetrating radar (GPR), among other geophysical methods, is used for quick determination of shallow stratigraphy – displaced, oblique layers within the fault zone. GPR data interpretation from diverse and complex reflection patterns of the fault zone heavily depends on the interpreter's experience. The range of different fault zone parameters in which this method can be successfully applied has not yet been investigated. We used a numerical simulation of GPR data to determine how GPR images the elements of faults (fault plane, hanging wall, footwall) in comparison with other reflections. Furthermore, we studied which parameters have the most significant impact on GPR wave patterns. We performed a series of numerical models of a fault, changing its geometry with increasing complexity from elementary models to realistic ones. The resulting synthetic profiles allowed finding specific GPR signatures from the fault plane, the hanging wall and the footwall. We collected field GPR data from two different fault zones and examined them for verification.

Ground-Penetrating Radar

Reflection

10.1002/nsg.12153

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Citations (13)

Adyr Faults: Generators of Strong Earthquakes in the Lake Issyk-Kul Depression (a Case Study of the Kultor Fault Zone)

Seismic Instruments (2020)

А. М. Корженков A. A. Strelnikov E. V. Deev L. A. Korzhenkova Jing Liu‐Zeng

10.3103/s0747923920050096

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Citations (5)