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Record #178260:

Evidence of late Pleistocene ice-dammed lake in West Siberia / Valery I. Astakhov.

Title: Evidence of late Pleistocene ice-dammed lake in West Siberia / Valery I. Astakhov.
Author(s): Astakhov, Valery I.
Date: 2006.
In: Boreas. (2006.), Vol. 35(4) (2006)
Abstract: Discusses geological data on proglacial lakes and spillways in West Siberian Plain, and crucial features of Late Pleistocene reorganization of drainage pattern of northern Eurasia. Focuses on sediments along margin of last ice sheet and south of it, including new data obtained by Russian-Norwegian research project PECHORA. Finds that margin of last ice sheet in western and central parts of West Siberia is localized above Arctic Circle (150-250 km north of previously suggested limit). Geochronological evidence indicates that last ice dam across West Siberia appeared at early stages of Weichselian ice age.
Notes:

Boreas. Vol. 35(4) :607-704 (2006).

Keywords: 551.32 -- Glaciology.
551.336 -- Ice ages.
551.337 -- Chronology of the Pleistocene and recent periods.
551.332.56 -- Lakes, ice-dammed. Glacial lakes. Disruption of water drainage.
550.93 -- Geochronology.
551.791 -- Pleistocene.
E7 -- Glaciology: glacial geology and ice ages.
(*501) -- Russia (Federation).
(*501.2) -- West Siberia.
SPRI record no.: 178260

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100 1# ‡aAstakhov, Valery I.
245 10 ‡aEvidence of late Pleistocene ice-dammed lake in West Siberia /‡cValery I. Astakhov.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2006.
300 ## ‡ap. 607-704 :‡bill., diags., tables, map.
500 ## ‡aBoreas. Vol. 35(4) :607-704 (2006).
520 3# ‡aDiscusses geological data on proglacial lakes and spillways in West Siberian Plain, and crucial features of Late Pleistocene reorganization of drainage pattern of northern Eurasia. Focuses on sediments along margin of last ice sheet and south of it, including new data obtained by Russian-Norwegian research project PECHORA. Finds that margin of last ice sheet in western and central parts of West Siberia is localized above Arctic Circle (150-250 km north of previously suggested limit). Geochronological evidence indicates that last ice dam across West Siberia appeared at early stages of Weichselian ice age.
530 ## ‡aAlso issued online ‡uurn:doi:10.1080/03009480600690845‡uhttps://dx.doi.org/10.1080/03009480600690845
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.337 -- Chronology of the Pleistocene and recent periods.‡2udc
650 07 ‡a551.332.56 -- Lakes, ice-dammed. Glacial lakes. Disruption of water drainage.‡2udc
650 07 ‡a550.93 -- Geochronology.‡2udc
650 07 ‡a551.791 -- Pleistocene.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*501) -- Russia (Federation).‡2udc
651 #7 ‡a(*501.2) -- West Siberia.‡2udc
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