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Record #96402:

Lofoten margin, North Norway: crustal structure adjacent to the ocean-continent transition / M.A. Sellevoll, I. Olafsson, M. Mokhtari, Arne Gidskehaug.

Title: Lofoten margin, North Norway: crustal structure adjacent to the ocean-continent transition / M.A. Sellevoll, I. Olafsson, M. Mokhtari, Arne Gidskehaug.
Author(s): Sellevoll, M. A.
Olafsson, I.
Mokhtari, M.
Gidskehaug, Arne.
Date: 1988.
In: Norges Geologiske Undersøkelse. Special Publication. (1988.), Vol. 3 (1988)
Abstract: Seismic reflection, refraction, magnetic and gravity measurements were made on Lofoten margin in 1982, to investigate crustal structure of area adjacent to assumed ocean-continental crustal transition. Results on landward side fo Vøring Plateau Escarpment indicate that Mesozoic basin is located below flow basalt covering continental slope off Lofoten. This and more southerly basins could be result of northern continuation of Rockall Trough rift system. Inter-crustal reflectors imply that transition is landward of seaward dipping sequence.
Notes:

Norges Geologiske Undersøkelse. Special Publication. Vol. 3 :39-48 (1988).

Keywords: 550.312 -- Gravity and isostasy.
550.389 -- Magnetic surveys.
550.834 -- Seismic survey methods.
551.1/.4 -- Geology.
551.462 -- Submarine topography, bottom forms.
551.76 -- Mesozoic.
552.323.5 -- Basalt.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*58) -- Norway.
SPRI record no.: 96402

MARCXML

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245 00 ‡aLofoten margin, North Norway :‡bcrustal structure adjacent to the ocean-continent transition /‡cM.A. Sellevoll, I. Olafsson, M. Mokhtari, Arne Gidskehaug.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1988.
300 ## ‡ap. 39-48 :‡bdiags., maps.
500 ## ‡aNorges Geologiske Undersøkelse. Special Publication. Vol. 3 :39-48 (1988).
520 3# ‡aSeismic reflection, refraction, magnetic and gravity measurements were made on Lofoten margin in 1982, to investigate crustal structure of area adjacent to assumed ocean-continental crustal transition. Results on landward side fo Vøring Plateau Escarpment indicate that Mesozoic basin is located below flow basalt covering continental slope off Lofoten. This and more southerly basins could be result of northern continuation of Rockall Trough rift system. Inter-crustal reflectors imply that transition is landward of seaward dipping sequence.
650 07 ‡a550.312 -- Gravity and isostasy.‡2udc
650 07 ‡a550.389 -- Magnetic surveys.‡2udc
650 07 ‡a550.834 -- Seismic survey methods.‡2udc
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.462 -- Submarine topography, bottom forms.‡2udc
650 07 ‡a551.76 -- Mesozoic.‡2udc
650 07 ‡a552.323.5 -- Basalt.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*58) -- Norway.‡2udc
700 1# ‡aSellevoll, M. A.
700 1# ‡aOlafsson, I.
700 1# ‡aMokhtari, M.
700 1# ‡aGidskehaug, Arne.
773 0# ‡7nnas ‡tNorges Geologiske Undersøkelse. Special Publication. ‡gVol. 3 (1988) ‡wSPRI-84344
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220925