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Record #122582:
Glacigenic deposits of the Central Deep: a key to the Late Quaternary evolution of the eastern Barents Sea / Valery Gataullin, Leonid Polyak, Oleg Epstein, Boris Romanyuk.
Title: | Glacigenic deposits of the Central Deep: a key to the Late Quaternary evolution of the eastern Barents Sea / Valery Gataullin, Leonid Polyak, Oleg Epstein, Boris Romanyuk. |
Author(s): | Gataullin, Valery. Polyak, Leonid. Epstein, Oleg. Romanyuk, Boris. |
Date: | 1993. |
In: | Boreas. (1993.), Vol. 22(1) (1993) |
Abstract: | Seismo-acoustic and shallow drilling data indicate that Quaternary deposits in this area are mainly composed of glacigenic sediments, comprising basal till and proximal and distal glaciomarine sediments deposited during last glacial cycle. Apparant glaciotectonic features imply strong glacial erosion of Mesozoic bedrock. General ice movement is assumed to have been from off Novaya Zemlya. Concludes that entire eastern Barents Sea was covered by Late Weichselian ice sheet. |
Notes: | Boreas. Vol. 22(1) :47-58 (1993). |
Keywords: | 551.336 -- Ice ages. 551.79 -- Quaternary. 551.33 -- Glacial geology. 551.332.25 -- Glacio-marine deposits. 551.332.212 -- Till or boulder clay. 551.332.2 -- Drift, glacial. Deposits. E7 -- Glaciology: glacial geology and ice ages. (*60) -- Arctic Ocean and adjacent waters. (*686) -- Barents Sea. |
SPRI record no.: | 122582 |
LDR 01610naa#a2200000#a#4500 001 SPRI-122582 005 20231201171949.0 007 ta 008 231201s1993####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-122582 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aGlacigenic deposits of the Central Deep :‡ba key to the Late Quaternary evolution of the eastern Barents Sea /‡cValery Gataullin, Leonid Polyak, Oleg Epstein, Boris Romanyuk. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1993. 300 ## ‡ap. 47-58 :‡bill., diag., maps. 500 ## ‡aBoreas. Vol. 22(1) :47-58 (1993). 520 3# ‡aSeismo-acoustic and shallow drilling data indicate that Quaternary deposits in this area are mainly composed of glacigenic sediments, comprising basal till and proximal and distal glaciomarine sediments deposited during last glacial cycle. Apparant glaciotectonic features imply strong glacial erosion of Mesozoic bedrock. General ice movement is assumed to have been from off Novaya Zemlya. Concludes that entire eastern Barents Sea was covered by Late Weichselian ice sheet. 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.332.25 -- Glacio-marine deposits.‡2udc 650 07 ‡a551.332.212 -- Till or boulder clay.‡2udc 650 07 ‡a551.332.2 -- Drift, glacial. Deposits.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*686) -- Barents Sea.‡2udc 700 1# ‡aGataullin, Valery. 700 1# ‡aPolyak, Leonid. 700 1# ‡aEpstein, Oleg. 700 1# ‡aRomanyuk, Boris. 773 0# ‡7nnas ‡tBoreas. ‡gVol. 22(1) (1993) ‡wSPRI-56035 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231201