Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Орография коренного рельефа района подледникового озера Восток (Восточная Антарктида). / Попов, С. В.; Лунёв, П. И.
в: ГЕОМОРФОЛОГИЯ, № 1, 03.12.2012, стр. 81-92.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Орография коренного рельефа района подледникового озера Восток (Восточная Антарктида)
AU - Попов, С. В.
AU - Лунёв, П. И.
PY - 2012/12/3
Y1 - 2012/12/3
N2 - On the base of topographic maps of 1 : 500 000 scale the regionalization of the territory was fulfilled. Three geomorphic regions were distinguished: 1 - the Vostok trench - submarine hilly plain of abs. height -900 m, with several depressions and rises; 2 - the Komsomolski mountains with abs. height up to 1580 m; 3 - the Shmidt plain with abs. height about 300 m and relief about 100 m. These regions are complexified by exogenic mesolandforms with different heights, depth of dissection and total morphology.
AB - On the base of topographic maps of 1 : 500 000 scale the regionalization of the territory was fulfilled. Three geomorphic regions were distinguished: 1 - the Vostok trench - submarine hilly plain of abs. height -900 m, with several depressions and rises; 2 - the Komsomolski mountains with abs. height up to 1580 m; 3 - the Shmidt plain with abs. height about 300 m and relief about 100 m. These regions are complexified by exogenic mesolandforms with different heights, depth of dissection and total morphology.
UR - http://www.scopus.com/inward/record.url?scp=84870161100&partnerID=8YFLogxK
UR - https://proxy.library.spbu.ru:2228/item.asp?id=17687491
M3 - статья
SP - 81
EP - 92
JO - ГЕОМОРФОЛОГИЯ
JF - ГЕОМОРФОЛОГИЯ
SN - 0435-4281
IS - 1
ER -
ID: 5462004