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Young Landforms Created by Earthquakes in the Foothills of the Kurai Range (Gorny Altai). / Korzhenkov, A. M.; Deev, E. V.; Pozdnyakova, N. I.

In: Seismic instruments, Vol. 58, No. 4, 03.08.2022, p. 424-441.

Research output: Contribution to journal › Article › peer-review

Harvard

Korzhenkov, AM, Deev, EV & Pozdnyakova, NI 2022, 'Young Landforms Created by Earthquakes in the Foothills of the Kurai Range (Gorny Altai)', Seismic instruments, vol. 58, no. 4, pp. 424-441. https://doi.org/10.3103/s0747923922040065

APA

Korzhenkov, A. M., Deev, E. V., & Pozdnyakova, N. I. (2022). Young Landforms Created by Earthquakes in the Foothills of the Kurai Range (Gorny Altai). Seismic instruments, 58(4), 424-441. https://doi.org/10.3103/s0747923922040065

Vancouver

Korzhenkov AM, Deev EV, Pozdnyakova NI. Young Landforms Created by Earthquakes in the Foothills of the Kurai Range (Gorny Altai). Seismic instruments. 2022 Aug 3;58(4):424-441. doi: 10.3103/s0747923922040065

Author

Korzhenkov, A. M. ; Deev, E. V. ; Pozdnyakova, N. I. / Young Landforms Created by Earthquakes in the Foothills of the Kurai Range (Gorny Altai). In: Seismic instruments. 2022 ; Vol. 58, No. 4. pp. 424-441.

BibTeX

@article{0d3b073766a24e30962d3c2238ffc17e,
title = "Young Landforms Created by Earthquakes in the Foothills of the Kurai Range (Gorny Altai)",
abstract = "Structural and geomorphological studies were carried out in the foothills of the Kurai Range in southeast Gorny Altai. It is shown that the structure of the Kurai Fault Zone here is governed by north-dipping reverse faults and thrusts, along which the Kurai Range thrusts onto deposits of the Chuya and Kurai depressions. They are feathered by south-dipping backthrusts. Displacements along these fault systems lead to growth of forbergs in front of the range front and separation of smaller negative morphostructures from the Chuya and Kurai depressions. Numerous fault scarps have been revealed along the faults, which are outlets of seismic sources of paleoearthquakes to the surface. For a number of scarps, in addition to the vertical component, the strike-slip component of displacements is also read in the relief. Some fault scarps have an age of a few hundred years and arose in the sources of paleoearthquakes with minimal magnitude: MW = 6.7–7.3.",
author = "Korzhenkov, {A. M.} and Deev, {E. V.} and Pozdnyakova, {N. I.}",
note = "The research was supported by the Russian Science Foundation (project no. 21-17-00058). Korzhenkov, A. M. Young Landforms Created by Earthquakes in the Foothills of the Kurai Range (Gorny Altai) / A. M. Korzhenkov, E. V. Deev, N. I. Pozdnyakova // Seismic Instruments. – 2022. – Vol. 58, No. 4. – P. 424-441. – DOI 10.3103/s0747923922040065. ",
year = "2022",
month = aug,
day = "3",
doi = "10.3103/s0747923922040065",
language = "English",
volume = "58",
pages = "424--441",
journal = "Seismic instruments",
issn = "0747-9239",
publisher = "Allerton Press Inc.",
number = "4",

}

RIS

TY - JOUR

T1 - Young Landforms Created by Earthquakes in the Foothills of the Kurai Range (Gorny Altai)

AU - Korzhenkov, A. M.

AU - Deev, E. V.

AU - Pozdnyakova, N. I.

N1 - The research was supported by the Russian Science Foundation (project no. 21-17-00058). Korzhenkov, A. M. Young Landforms Created by Earthquakes in the Foothills of the Kurai Range (Gorny Altai) / A. M. Korzhenkov, E. V. Deev, N. I. Pozdnyakova // Seismic Instruments. – 2022. – Vol. 58, No. 4. – P. 424-441. – DOI 10.3103/s0747923922040065.

PY - 2022/8/3

Y1 - 2022/8/3

N2 - Structural and geomorphological studies were carried out in the foothills of the Kurai Range in southeast Gorny Altai. It is shown that the structure of the Kurai Fault Zone here is governed by north-dipping reverse faults and thrusts, along which the Kurai Range thrusts onto deposits of the Chuya and Kurai depressions. They are feathered by south-dipping backthrusts. Displacements along these fault systems lead to growth of forbergs in front of the range front and separation of smaller negative morphostructures from the Chuya and Kurai depressions. Numerous fault scarps have been revealed along the faults, which are outlets of seismic sources of paleoearthquakes to the surface. For a number of scarps, in addition to the vertical component, the strike-slip component of displacements is also read in the relief. Some fault scarps have an age of a few hundred years and arose in the sources of paleoearthquakes with minimal magnitude: MW = 6.7–7.3.

AB - Structural and geomorphological studies were carried out in the foothills of the Kurai Range in southeast Gorny Altai. It is shown that the structure of the Kurai Fault Zone here is governed by north-dipping reverse faults and thrusts, along which the Kurai Range thrusts onto deposits of the Chuya and Kurai depressions. They are feathered by south-dipping backthrusts. Displacements along these fault systems lead to growth of forbergs in front of the range front and separation of smaller negative morphostructures from the Chuya and Kurai depressions. Numerous fault scarps have been revealed along the faults, which are outlets of seismic sources of paleoearthquakes to the surface. For a number of scarps, in addition to the vertical component, the strike-slip component of displacements is also read in the relief. Some fault scarps have an age of a few hundred years and arose in the sources of paleoearthquakes with minimal magnitude: MW = 6.7–7.3.

UR - https://www.mendeley.com/catalogue/65c8c9cd-8cfc-3efb-8b68-50874ed7d7b9/

UR - https://www.elibrary.ru/item.asp?id=57734849

U2 - 10.3103/s0747923922040065

DO - 10.3103/s0747923922040065

M3 - Article

VL - 58

SP - 424

EP - 441

JO - Seismic instruments

JF - Seismic instruments

SN - 0747-9239

IS - 4

ER -

ID: 68318478