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Geomorphological criteria for the reconstruction of late pleistocene ice caps in northern eurasia. / Makkaveyev, A. N.; Aseyev, A. A.; Astakhov, V. I.; Bronguleyev, V.; Isayeva, L. L.; Lavrov, A. S.; Matishov, G. G.

In: Polar Geography and Geology, Vol. 6, No. 1, 01.01.1982, p. 25-41.

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

Harvard

Makkaveyev, AN, Aseyev, AA, Astakhov, VI, Bronguleyev, V, Isayeva, LL, Lavrov, AS & Matishov, GG 1982, 'Geomorphological criteria for the reconstruction of late pleistocene ice caps in northern eurasia', Polar Geography and Geology, vol. 6, no. 1, pp. 25-41. https://doi.org/10.1080/10889378209377151

APA

Makkaveyev, A. N., Aseyev, A. A., Astakhov, V. I., Bronguleyev, V., Isayeva, L. L., Lavrov, A. S., & Matishov, G. G. (1982). Geomorphological criteria for the reconstruction of late pleistocene ice caps in northern eurasia. Polar Geography and Geology, 6(1), 25-41. https://doi.org/10.1080/10889378209377151

Vancouver

Makkaveyev AN, Aseyev AA, Astakhov VI, Bronguleyev V, Isayeva LL, Lavrov AS et al. Geomorphological criteria for the reconstruction of late pleistocene ice caps in northern eurasia. Polar Geography and Geology. 1982 Jan 1;6(1):25-41. https://doi.org/10.1080/10889378209377151

Author

Makkaveyev, A. N. ; Aseyev, A. A. ; Astakhov, V. I. ; Bronguleyev, V. ; Isayeva, L. L. ; Lavrov, A. S. ; Matishov, G. G. / Geomorphological criteria for the reconstruction of late pleistocene ice caps in northern eurasia. In: Polar Geography and Geology. 1982 ; Vol. 6, No. 1. pp. 25-41.

BibTeX

@article{e35a0982c3ee4925b3355c73a32f01ae,
title = "Geomorphological criteria for the reconstruction of late pleistocene ice caps in northern eurasia",
abstract = "The positions of ice dispersal centers and of ice cap limits, both on land and on the sea bed, have been located fairly precisely by means of an analysis of marginal features produced by the last glaciation of Northern Eurasia, using in particular new data on the geomorphology of the beds of the Barents and Kara seas. The configuration of the various ice caps was then reconstructed on the basis of both glaciological and geomorphological data. Of particular interest is the conclusion that both the Barents and Kara seas were covered by a number of independent ice caps, contiguous to varying degrees and for verying periods, rather than by one massive ice cap, as had been earlier proposed. (The translation is by William Barr, University of Saskatchewan, Saskatoon.).",
author = "Makkaveyev, {A. N.} and Aseyev, {A. A.} and Astakhov, {V. I.} and V. Bronguleyev and Isayeva, {L. L.} and Lavrov, {A. S.} and Matishov, {G. G.}",
year = "1982",
month = jan,
day = "1",
doi = "10.1080/10889378209377151",
language = "English",
volume = "6",
pages = "25--41",
journal = "Polar Geography",
issn = "1088-937X",
publisher = "Taylor & Francis",
number = "1",

}

RIS

TY - JOUR

T1 - Geomorphological criteria for the reconstruction of late pleistocene ice caps in northern eurasia

AU - Makkaveyev, A. N.

AU - Aseyev, A. A.

AU - Astakhov, V. I.

AU - Bronguleyev, V.

AU - Isayeva, L. L.

AU - Lavrov, A. S.

AU - Matishov, G. G.

PY - 1982/1/1

Y1 - 1982/1/1

N2 - The positions of ice dispersal centers and of ice cap limits, both on land and on the sea bed, have been located fairly precisely by means of an analysis of marginal features produced by the last glaciation of Northern Eurasia, using in particular new data on the geomorphology of the beds of the Barents and Kara seas. The configuration of the various ice caps was then reconstructed on the basis of both glaciological and geomorphological data. Of particular interest is the conclusion that both the Barents and Kara seas were covered by a number of independent ice caps, contiguous to varying degrees and for verying periods, rather than by one massive ice cap, as had been earlier proposed. (The translation is by William Barr, University of Saskatchewan, Saskatoon.).

AB - The positions of ice dispersal centers and of ice cap limits, both on land and on the sea bed, have been located fairly precisely by means of an analysis of marginal features produced by the last glaciation of Northern Eurasia, using in particular new data on the geomorphology of the beds of the Barents and Kara seas. The configuration of the various ice caps was then reconstructed on the basis of both glaciological and geomorphological data. Of particular interest is the conclusion that both the Barents and Kara seas were covered by a number of independent ice caps, contiguous to varying degrees and for verying periods, rather than by one massive ice cap, as had been earlier proposed. (The translation is by William Barr, University of Saskatchewan, Saskatoon.).

UR - http://www.scopus.com/inward/record.url?scp=0009587786&partnerID=8YFLogxK

U2 - 10.1080/10889378209377151

DO - 10.1080/10889378209377151

M3 - Article

AN - SCOPUS:0009587786

VL - 6

SP - 25

EP - 41

JO - Polar Geography

JF - Polar Geography

SN - 1088-937X

IS - 1

ER -

ID: 53753079