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КЛИНОВИДНЫЕ СТРУКТУРЫ В РЫХЛЫХ ОТЛОЖЕНИЯХ ПРИНЕВСКОЙ НИЗМЕННОСТИ КАК СЛЕДСТВИЕ СЕЙСМИЧЕСКИХ ВОЗДЕЙСТВИЙ В РАННЕМ ГОЛОЦЕНЕ : (ОПОРНЫЙ УЧАСТОК “НИЗИНО”). / Shvarev, S. V.; Nikonov, A. A.; Rusakov, A. V.

In: ГЕОМОРФОЛОГИЯ, Vol. 2018-January, No. 2, 01.01.2018, p. 99-114.

Research output: Contribution to journal › Review article › peer-review

Harvard

Shvarev, SV, Nikonov, AA & Rusakov, AV 2018, 'КЛИНОВИДНЫЕ СТРУКТУРЫ В РЫХЛЫХ ОТЛОЖЕНИЯХ ПРИНЕВСКОЙ НИЗМЕННОСТИ КАК СЛЕДСТВИЕ СЕЙСМИЧЕСКИХ ВОЗДЕЙСТВИЙ В РАННЕМ ГОЛОЦЕНЕ: (ОПОРНЫЙ УЧАСТОК “НИЗИНО”)', ГЕОМОРФОЛОГИЯ, vol. 2018-January, no. 2, pp. 99-114. https://doi.org/10.7868/S0435428118020086

APA

Shvarev, S. V., Nikonov, A. A., & Rusakov, A. V. (2018). КЛИНОВИДНЫЕ СТРУКТУРЫ В РЫХЛЫХ ОТЛОЖЕНИЯХ ПРИНЕВСКОЙ НИЗМЕННОСТИ КАК СЛЕДСТВИЕ СЕЙСМИЧЕСКИХ ВОЗДЕЙСТВИЙ В РАННЕМ ГОЛОЦЕНЕ: (ОПОРНЫЙ УЧАСТОК “НИЗИНО”). ГЕОМОРФОЛОГИЯ, 2018-January(2), 99-114. https://doi.org/10.7868/S0435428118020086

Vancouver

Shvarev SV, Nikonov AA, Rusakov AV. КЛИНОВИДНЫЕ СТРУКТУРЫ В РЫХЛЫХ ОТЛОЖЕНИЯХ ПРИНЕВСКОЙ НИЗМЕННОСТИ КАК СЛЕДСТВИЕ СЕЙСМИЧЕСКИХ ВОЗДЕЙСТВИЙ В РАННЕМ ГОЛОЦЕНЕ: (ОПОРНЫЙ УЧАСТОК “НИЗИНО”). ГЕОМОРФОЛОГИЯ. 2018 Jan 1;2018-January(2):99-114. https://doi.org/10.7868/S0435428118020086

Author

Shvarev, S. V. ; Nikonov, A. A. ; Rusakov, A. V. / КЛИНОВИДНЫЕ СТРУКТУРЫ В РЫХЛЫХ ОТЛОЖЕНИЯХ ПРИНЕВСКОЙ НИЗМЕННОСТИ КАК СЛЕДСТВИЕ СЕЙСМИЧЕСКИХ ВОЗДЕЙСТВИЙ В РАННЕМ ГОЛОЦЕНЕ : (ОПОРНЫЙ УЧАСТОК “НИЗИНО”). In: ГЕОМОРФОЛОГИЯ. 2018 ; Vol. 2018-January, No. 2. pp. 99-114.

BibTeX

@article{4604eb4c25504149a7825af73dbb3bad,
title = "КЛИНОВИДНЫЕ СТРУКТУРЫ В РЫХЛЫХ ОТЛОЖЕНИЯХ ПРИНЕВСКОЙ НИЗМЕННОСТИ КАК СЛЕДСТВИЕ СЕЙСМИЧЕСКИХ ВОЗДЕЙСТВИЙ В РАННЕМ ГОЛОЦЕНЕ: (ОПОРНЫЙ УЧАСТОК “НИЗИНО”)",
abstract = "The article discusses the origin of wedge-shaped structures observed on southern lowland of the Gulf of Finland near the village of Nizino in 2000-2005 and 2014. Obtained results confirm the seismic origin of the wedges. Morphological characteristics, nature and consistency of the filling, deformation of the enclosing strata show the instant disclosure, a quick one-act filling cavities with material from the sides and roof, the subsequent momentary closure with compression in connection with the directed lateral dynamic effects. In addition, we analyzed the distribution of various deformation structures in Paleozoic rocks and postglacial sediments within this region and arrived to the conclusion about their structural control and paleoseismic origin.",
keywords = "Fennoscandian shield, Holocene, Neva Lowland, Postglacial deposits, Seismogenic deformations, Wedge-shaped structures",
author = "Shvarev, {S. V.} and Nikonov, {A. A.} and Rusakov, {A. V.}",
year = "2018",
month = jan,
day = "1",
doi = "10.7868/S0435428118020086",
language = "русский",
volume = "2018-January",
pages = "99--114",
journal = "ГЕОМОРФОЛОГИЯ",
issn = "0435-4281",
publisher = "Российская академия наук",
number = "2",

}

RIS

TY - JOUR

T1 - КЛИНОВИДНЫЕ СТРУКТУРЫ В РЫХЛЫХ ОТЛОЖЕНИЯХ ПРИНЕВСКОЙ НИЗМЕННОСТИ КАК СЛЕДСТВИЕ СЕЙСМИЧЕСКИХ ВОЗДЕЙСТВИЙ В РАННЕМ ГОЛОЦЕНЕ

T2 - (ОПОРНЫЙ УЧАСТОК “НИЗИНО”)

AU - Shvarev, S. V.

AU - Nikonov, A. A.

AU - Rusakov, A. V.

PY - 2018/1/1

Y1 - 2018/1/1

N2 - The article discusses the origin of wedge-shaped structures observed on southern lowland of the Gulf of Finland near the village of Nizino in 2000-2005 and 2014. Obtained results confirm the seismic origin of the wedges. Morphological characteristics, nature and consistency of the filling, deformation of the enclosing strata show the instant disclosure, a quick one-act filling cavities with material from the sides and roof, the subsequent momentary closure with compression in connection with the directed lateral dynamic effects. In addition, we analyzed the distribution of various deformation structures in Paleozoic rocks and postglacial sediments within this region and arrived to the conclusion about their structural control and paleoseismic origin.

AB - The article discusses the origin of wedge-shaped structures observed on southern lowland of the Gulf of Finland near the village of Nizino in 2000-2005 and 2014. Obtained results confirm the seismic origin of the wedges. Morphological characteristics, nature and consistency of the filling, deformation of the enclosing strata show the instant disclosure, a quick one-act filling cavities with material from the sides and roof, the subsequent momentary closure with compression in connection with the directed lateral dynamic effects. In addition, we analyzed the distribution of various deformation structures in Paleozoic rocks and postglacial sediments within this region and arrived to the conclusion about their structural control and paleoseismic origin.

KW - Fennoscandian shield

KW - Holocene

KW - Neva Lowland

KW - Postglacial deposits

KW - Seismogenic deformations

KW - Wedge-shaped structures

UR - http://www.scopus.com/inward/record.url?scp=85056534486&partnerID=8YFLogxK

U2 - 10.7868/S0435428118020086

DO - 10.7868/S0435428118020086

M3 - Обзорная статья

AN - SCOPUS:85056534486

VL - 2018-January

SP - 99

EP - 114

JO - ГЕОМОРФОЛОГИЯ

JF - ГЕОМОРФОЛОГИЯ

SN - 0435-4281

IS - 2

ER -

ID: 38217219