skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View a record

Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.

Please search for material in iDiscover for up-to-date information about the library collection.


Record #88145:

The geological implications of the upper seismic unit, southeastern Barents Sea / Joar Saettem, Martin Hamborg.

Title: The geological implications of the upper seismic unit, southeastern Barents Sea / Joar Saettem, Martin Hamborg.
Author(s): Saettem, Joar.
Hamborg, Martin.
Date: 1987.
In: Polar Research. (1987.), Vol. 5(3) (1987)
Abstract: Upper Quaternary seismic unit mapped. Sediments in unit interpreted as of glaciogenic origin and most likely consisting of till.
Notes:

Polar Research. Vol. 5(3) :298-301 (1987).

Keywords: 551.352/.353 -- Marine sediments, deep sea.
551.332 -- Glacial deposition.
B -- Geology and soil sciences.
(*686) -- Barents Sea.
SPRI record no.: 88145

MARCXML

LDR 00919naa#a2200000#a#4500
001 SPRI-88145
005 20231003190558.0
007 ta
008 231003s1987####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-88145
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aSaettem, Joar.
245 14 ‡aThe geological implications of the upper seismic unit, southeastern Barents Sea /‡cJoar Saettem, Martin Hamborg.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1987.
300 ## ‡ap. 298-301 :‡bdiag., maps.
500 ## ‡aPolar Research. Vol. 5(3) :298-301 (1987).
520 3# ‡aUpper Quaternary seismic unit mapped. Sediments in unit interpreted as of glaciogenic origin and most likely consisting of till.
650 07 ‡a551.352/.353 -- Marine sediments, deep sea.‡2udc
650 07 ‡a551.332 -- Glacial deposition.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*686) -- Barents Sea.‡2udc
700 1# ‡aHamborg, Martin.
773 0# ‡7nnas ‡tPolar Research. ‡gVol. 5(3) (1987) ‡wSPRI-64246
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20231003