Investigations of north Caucasus landslides and antilandslide design development › Научные исследования в СПбГУ

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Investigations of north Caucasus landslides and antilandslide design development. / Shadunts, K. S.; Matsiy, S. I.; Zhirov, A. I.; Zabuldin, B. V.

Engineering geology and the environment. Proc. symposium, Athens, 1997, vol.1. vol.1. ред. 1997. стр. 1037-1041.

Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференций › статья в сборнике материалов конференции › научная › Рецензирование

Harvard

Shadunts, KS, Matsiy, SI, Zhirov, AI & Zabuldin, BV 1997, Investigations of north Caucasus landslides and antilandslide design development. в Engineering geology and the environment. Proc. symposium, Athens, 1997, vol.1. vol.1 изд., стр. 1037-1041.

APA

Shadunts, K. S., Matsiy, S. I., Zhirov, A. I., & Zabuldin, B. V. (1997). Investigations of north Caucasus landslides and antilandslide design development. в Engineering geology and the environment. Proc. symposium, Athens, 1997, vol.1 (vol.1 ред., стр. 1037-1041)

Vancouver

Shadunts KS, Matsiy SI, Zhirov AI, Zabuldin BV. Investigations of north Caucasus landslides and antilandslide design development. в Engineering geology and the environment. Proc. symposium, Athens, 1997, vol.1. vol.1 ред. 1997. стр. 1037-1041

Author

Shadunts, K. S. ; Matsiy, S. I. ; Zhirov, A. I. ; Zabuldin, B. V. / Investigations of north Caucasus landslides and antilandslide design development. Engineering geology and the environment. Proc. symposium, Athens, 1997, vol.1. vol.1. ред. 1997. стр. 1037-1041

BibTeX

@inproceedings{431efdfa24194b73b71684f0f2c20d53,

title = "Investigations of north Caucasus landslides and antilandslide design development",

abstract = "Landslides in the North Caucasus occur in rocks of different geological age and types. Landslide processes are attributed to the clay rocks of certain horizons - from loams of Quaternary age to shales of the middle Jura. The specific character of a landslide in clay rocks of different lithification degree is that as the surface layer is displaced a new sliding surface is formed. One of the landslides has destroyed oil-pipeline. The landslide massif is frontier, its length - 140-210m, width -320m, slope angle - up to 35°. To stabilise the landslide antilandslide measures have been developed and they include: 1) the supporting construction which presents a pile row (800mm in diameter) placed at the bottom side of the pipeline shelf; 2) original anchor constructions supporting surface hearths; 3) river anti-wash-out measures, involving overflow dam constructions of large stone and anchored brushwood bundles.",

author = "Shadunts, {K. S.} and Matsiy, {S. I.} and Zhirov, {A. I.} and Zabuldin, {B. V.}",

year = "1997",

language = "English",

pages = "1037--1041",

booktitle = "Engineering geology and the environment. Proc. symposium, Athens, 1997, vol.1",

edition = "vol.1",

}

RIS

TY - GEN

T1 - Investigations of north Caucasus landslides and antilandslide design development

AU - Shadunts, K. S.

AU - Matsiy, S. I.

AU - Zhirov, A. I.

AU - Zabuldin, B. V.

PY - 1997

Y1 - 1997

N2 - Landslides in the North Caucasus occur in rocks of different geological age and types. Landslide processes are attributed to the clay rocks of certain horizons - from loams of Quaternary age to shales of the middle Jura. The specific character of a landslide in clay rocks of different lithification degree is that as the surface layer is displaced a new sliding surface is formed. One of the landslides has destroyed oil-pipeline. The landslide massif is frontier, its length - 140-210m, width -320m, slope angle - up to 35°. To stabilise the landslide antilandslide measures have been developed and they include: 1) the supporting construction which presents a pile row (800mm in diameter) placed at the bottom side of the pipeline shelf; 2) original anchor constructions supporting surface hearths; 3) river anti-wash-out measures, involving overflow dam constructions of large stone and anchored brushwood bundles.

AB - Landslides in the North Caucasus occur in rocks of different geological age and types. Landslide processes are attributed to the clay rocks of certain horizons - from loams of Quaternary age to shales of the middle Jura. The specific character of a landslide in clay rocks of different lithification degree is that as the surface layer is displaced a new sliding surface is formed. One of the landslides has destroyed oil-pipeline. The landslide massif is frontier, its length - 140-210m, width -320m, slope angle - up to 35°. To stabilise the landslide antilandslide measures have been developed and they include: 1) the supporting construction which presents a pile row (800mm in diameter) placed at the bottom side of the pipeline shelf; 2) original anchor constructions supporting surface hearths; 3) river anti-wash-out measures, involving overflow dam constructions of large stone and anchored brushwood bundles.

UR - http://www.scopus.com/inward/record.url?scp=0031432289&partnerID=8YFLogxK

M3 - Conference contribution

AN - SCOPUS:0031432289

SP - 1037

EP - 1041

BT - Engineering geology and the environment. Proc. symposium, Athens, 1997, vol.1

ER -

ID: 70039417