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Technique and results of geomorphologic mapping of submarine-subglacial relief of Lambert Basin and its frame (Eastern Antarctica). / Lastochkin, A. N.; Popov, S. V.

In: Geomorfologiya, No. 2, 01.01.2002, p. 80-91.

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

Harvard

Lastochkin, AN & Popov, SV 2002, 'Technique and results of geomorphologic mapping of submarine-subglacial relief of Lambert Basin and its frame (Eastern Antarctica)', Geomorfologiya, no. 2, pp. 80-91.

APA

Lastochkin, A. N., & Popov, S. V. (2002). Technique and results of geomorphologic mapping of submarine-subglacial relief of Lambert Basin and its frame (Eastern Antarctica). Geomorfologiya, (2), 80-91.

Vancouver

Lastochkin AN, Popov SV. Technique and results of geomorphologic mapping of submarine-subglacial relief of Lambert Basin and its frame (Eastern Antarctica). Geomorfologiya. 2002 Jan 1;(2):80-91.

Author

Lastochkin, A. N. ; Popov, S. V. / Technique and results of geomorphologic mapping of submarine-subglacial relief of Lambert Basin and its frame (Eastern Antarctica). In: Geomorfologiya. 2002 ; No. 2. pp. 80-91.

BibTeX

@article{ac30574acc3d445eb945bbaef4030a82,
title = "Technique and results of geomorphologic mapping of submarine-subglacial relief of Lambert Basin and its frame (Eastern Antarctica)",
abstract = "Complex geophysical researches including radiolocation profiling, terrestrial and marine seismic survey fulfilled during the 17-19, 32, 33, 35, 36, 39 and 40th Soviet (Russian) Antarctic expeditions made is possible to investigate the submarine-subglacial sea bottom relief in the vicinity of Prince Charles Mountains. The schematic geomorphologic map was compiled in the scale of 1 : 1000000, on the base of the morphogenetic principle. The map includes 6 genetic and 11 morphologic classes of simple surfaces, divided by crest and keel lines, concave and convex kinks. Within the submarine middle-mountains there are deep incised canyons, on the high plain - rare troughs and circles possibly buried by moraines. The Lambert depression has flat bottom and dissected flanges of various slopes. On the whole the submarine-subglacial relief greatly differs from the relief of Pleistocene glaciations.",
author = "Lastochkin, {A. N.} and Popov, {S. V.}",
year = "2002",
month = jan,
day = "1",
language = "русский",
pages = "80--91",
journal = "ГЕОМОРФОЛОГИЯ",
issn = "0435-4281",
publisher = "Российская академия наук",
number = "2",

}

RIS

TY - JOUR

T1 - Technique and results of geomorphologic mapping of submarine-subglacial relief of Lambert Basin and its frame (Eastern Antarctica)

AU - Lastochkin, A. N.

AU - Popov, S. V.

PY - 2002/1/1

Y1 - 2002/1/1

N2 - Complex geophysical researches including radiolocation profiling, terrestrial and marine seismic survey fulfilled during the 17-19, 32, 33, 35, 36, 39 and 40th Soviet (Russian) Antarctic expeditions made is possible to investigate the submarine-subglacial sea bottom relief in the vicinity of Prince Charles Mountains. The schematic geomorphologic map was compiled in the scale of 1 : 1000000, on the base of the morphogenetic principle. The map includes 6 genetic and 11 morphologic classes of simple surfaces, divided by crest and keel lines, concave and convex kinks. Within the submarine middle-mountains there are deep incised canyons, on the high plain - rare troughs and circles possibly buried by moraines. The Lambert depression has flat bottom and dissected flanges of various slopes. On the whole the submarine-subglacial relief greatly differs from the relief of Pleistocene glaciations.

AB - Complex geophysical researches including radiolocation profiling, terrestrial and marine seismic survey fulfilled during the 17-19, 32, 33, 35, 36, 39 and 40th Soviet (Russian) Antarctic expeditions made is possible to investigate the submarine-subglacial sea bottom relief in the vicinity of Prince Charles Mountains. The schematic geomorphologic map was compiled in the scale of 1 : 1000000, on the base of the morphogenetic principle. The map includes 6 genetic and 11 morphologic classes of simple surfaces, divided by crest and keel lines, concave and convex kinks. Within the submarine middle-mountains there are deep incised canyons, on the high plain - rare troughs and circles possibly buried by moraines. The Lambert depression has flat bottom and dissected flanges of various slopes. On the whole the submarine-subglacial relief greatly differs from the relief of Pleistocene glaciations.

UR - http://www.scopus.com/inward/record.url?scp=0036081611&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0036081611

SP - 80

EP - 91

JO - ГЕОМОРФОЛОГИЯ

JF - ГЕОМОРФОЛОГИЯ

SN - 0435-4281

IS - 2

ER -

ID: 36671236