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Record #189215:

Weichselian glacial stage in Murchison fjorden, Nordauslandet, Svalbard / Anu Kaakinen, and 4 others.

Title: Weichselian glacial stage in Murchison fjorden, Nordauslandet, Svalbard / Anu Kaakinen, and 4 others.
Author(s): Kaakinen, Anu.
Date: 2009.
In: Boreas. (2009.), Vol. 38(4) (2009)
Abstract: Presents new results from glacial geological, sedimentological and chronological studies in southern Murchisonfjorden area. Field data include reconnaissance mapping and detailed logging of vertical sectors along cliff-face outcrops adjacent to present shoreline. Compared with optically stimulated luminescence and accelerator mass spectrometry age determinations, data provide evidence of three successive Weichselian sequences, each represented by deposition of till followed by accumulation of shallow marine deposits. Contrary to earlier conclusions, study demonstrates that area was occupied by Late Weichselian glacier (LWG), though LWG till is thin and discontinuous.
Notes:

Boreas. Vol. 38(4) :718-729 (2009).

Keywords: 551.1/.4 -- Geology.
528 -- Geodesy.
551.3.051 -- Sedimentation and stratification.
551.332 -- Glacial deposition.
551.336 -- Ice ages.
551.337 -- Chronology of the Pleistocene and recent periods.
551.794 -- Holocene.
E7 -- Glaciology: glacial geology and ice ages.
(*3) -- Arctic regions.
(*32) -- Svalbard.
SPRI record no.: 189215

MARCXML

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001 SPRI-189215
005 20240329133543.0
007 ta
008 240329s2009####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-189215
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aKaakinen, Anu.
245 10 ‡aWeichselian glacial stage in Murchison fjorden, Nordauslandet, Svalbard /‡cAnu Kaakinen, and 4 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2009.
300 ## ‡ap. 718-729 :‡bill., diags., table, maps.
500 ## ‡aBoreas. Vol. 38(4) :718-729 (2009).
520 3# ‡aPresents new results from glacial geological, sedimentological and chronological studies in southern Murchisonfjorden area. Field data include reconnaissance mapping and detailed logging of vertical sectors along cliff-face outcrops adjacent to present shoreline. Compared with optically stimulated luminescence and accelerator mass spectrometry age determinations, data provide evidence of three successive Weichselian sequences, each represented by deposition of till followed by accumulation of shallow marine deposits. Contrary to earlier conclusions, study demonstrates that area was occupied by Late Weichselian glacier (LWG), though LWG till is thin and discontinuous.
530 ## ‡aAlso issued online ‡uurn:doi:10.1111/j.1502-3885.2009.00092.x‡uhttps://dx.doi.org/10.1111/j.1502-3885.2009.00092.x
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a528 -- Geodesy.‡2udc
650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc
650 07 ‡a551.332 -- Glacial deposition.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.337 -- Chronology of the Pleistocene and recent periods.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*32) -- Svalbard.‡2udc
773 0# ‡7nnas ‡tBoreas. ‡gVol. 38(4) (2009) ‡wSPRI-56035
916 ## ‡aJW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240329 ‡bJW