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Record #107363:

Crustal structure of the sheared southwestern Barents Sea continental margin / H.R. Jackson, Jan Inge Faleide, O. Eldholm.

Title: Crustal structure of the sheared southwestern Barents Sea continental margin / H.R. Jackson, Jan Inge Faleide, O. Eldholm.
Author(s): Jackson, H. R.
Faleide, Jan Inge.
Eldholm, O.
Date: 1990.
Abstract: Eighteen expanding spread profiles (collected 1983-86) were studied with seismic interpretation techniques and in conjunction with seismic reflection data. Results showed oceanic crust at Senja Fracture Zone to differ from standard oceanic crust, with velocity for layer 2 of 5.7-6.4 km s⁻¹ and slightly smaller crystalline crustal thickness. Continent-ocean transition at crustal depths was in range of 10-20 km. Depths down to 20 km were inferred for base of sedimentary section in south-western Barents Sea.
Notes:

Offprint: Marine Geology. Vol. 93 :119-146.

Keywords: 550.3 -- Geophysics.
550.834 -- Seismic survey methods.
551.1/.4(26) -- Marine geology.
551.24 -- Geotectonics.
551.46 -- Oceanography, physical.
551.462 -- Submarine topography, bottom forms.
551.462.32 -- Continental shelves.
B -- Geology and soil sciences.
(*60) -- Arctic Ocean and adjacent waters.
(*686) -- Barents Sea.
Location(s): SCO: SPRI-SHF: (*60) : 55
SPRI record no.: 107363

MARCXML

LDR 01637nam#a2200000#a#4500
001 SPRI-107363
005 20221003190654.0
007 ta
008 221003s1990####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-107363
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aJackson, H. R.
245 10 ‡aCrustal structure of the sheared southwestern Barents Sea continental margin /‡cH.R. Jackson, Jan Inge Faleide, O. Eldholm.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1990.
300 ## ‡ap. 119-146 :‡bdiags., tables, map.
500 ## ‡aOffprint: Marine Geology. Vol. 93 :119-146.
520 3# ‡aEighteen expanding spread profiles (collected 1983-86) were studied with seismic interpretation techniques and in conjunction with seismic reflection data. Results showed oceanic crust at Senja Fracture Zone to differ from standard oceanic crust, with velocity for layer 2 of 5.7-6.4 km s⁻¹ and slightly smaller crystalline crustal thickness. Continent-ocean transition at crustal depths was in range of 10-20 km. Depths down to 20 km were inferred for base of sedimentary section in south-western Barents Sea.
650 07 ‡a550.3 -- Geophysics.‡2udc
650 07 ‡a550.834 -- Seismic survey methods.‡2udc
650 07 ‡a551.1/.4(26) -- Marine geology.‡2udc
650 07 ‡a551.24 -- Geotectonics.‡2udc
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.462 -- Submarine topography, bottom forms.‡2udc
650 07 ‡a551.462.32 -- Continental shelves.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*686) -- Barents Sea.‡2udc
700 1# ‡aFaleide, Jan Inge.
700 1# ‡aEldholm, O.
852 7# ‡2camdept‡bSCO‡cSPRI-SHF‡h(*60) : 55‡9Create 1 item record‡0Migrate
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221003