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Subglacial relief of the central part of East Antarctica (According to data of abris project). / Popov, S. V.; Леонов, Вадим Олегович.

в: Geomorfologiya, № 3, 08.10.2009, стр. 100-111.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Popov, SV & Леонов, ВО 2009, 'Subglacial relief of the central part of East Antarctica (According to data of abris project)', Geomorfologiya, № 3, стр. 100-111.

APA

Popov, S. V., & Леонов, В. О. (2009). Subglacial relief of the central part of East Antarctica (According to data of abris project). Geomorfologiya, (3), 100-111.

Vancouver

Popov SV, Леонов ВО. Subglacial relief of the central part of East Antarctica (According to data of abris project). Geomorfologiya. 2009 Окт. 8;(3):100-111.

Author

Popov, S. V. ; Леонов, Вадим Олегович. / Subglacial relief of the central part of East Antarctica (According to data of abris project). в: Geomorfologiya. 2009 ; № 3. стр. 100-111.

BibTeX

@article{78bc8f0ecb8f49798643aa885c820ff9,
title = "Subglacial relief of the central part of East Antarctica (According to data of abris project)",
abstract = "The East Antarctica may be subdivided into 5 regions: basins and troughs (<-100 m), plains (-100-400 m), hills (400-1000 m), low mountains (1000-1500 m), middle mountains (>1500 m). There are evidences of at least two stages of subglacial relief formation. The first stage corresponds to platform type development with weak tectonic activity. The second one is characteristic of mobile folded zones where tectonic movements had large amplitudes and strong spatial differentiation (especially during Cenozoic era).",
author = "Popov, {S. V.} and Леонов, {Вадим Олегович}",
year = "2009",
month = oct,
day = "8",
language = "English",
pages = "100--111",
journal = "ГЕОМОРФОЛОГИЯ",
issn = "0435-4281",
publisher = "Российская академия наук",
number = "3",

}

RIS

TY - JOUR

T1 - Subglacial relief of the central part of East Antarctica (According to data of abris project)

AU - Popov, S. V.

AU - Леонов, Вадим Олегович

PY - 2009/10/8

Y1 - 2009/10/8

N2 - The East Antarctica may be subdivided into 5 regions: basins and troughs (<-100 m), plains (-100-400 m), hills (400-1000 m), low mountains (1000-1500 m), middle mountains (>1500 m). There are evidences of at least two stages of subglacial relief formation. The first stage corresponds to platform type development with weak tectonic activity. The second one is characteristic of mobile folded zones where tectonic movements had large amplitudes and strong spatial differentiation (especially during Cenozoic era).

AB - The East Antarctica may be subdivided into 5 regions: basins and troughs (<-100 m), plains (-100-400 m), hills (400-1000 m), low mountains (1000-1500 m), middle mountains (>1500 m). There are evidences of at least two stages of subglacial relief formation. The first stage corresponds to platform type development with weak tectonic activity. The second one is characteristic of mobile folded zones where tectonic movements had large amplitudes and strong spatial differentiation (especially during Cenozoic era).

UR - http://www.scopus.com/inward/record.url?scp=70349626249&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:70349626249

SP - 100

EP - 111

JO - ГЕОМОРФОЛОГИЯ

JF - ГЕОМОРФОЛОГИЯ

SN - 0435-4281

IS - 3

ER -

ID: 36670668