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Record #96403:
- #96403
Main publication details
MARC recordResults of two seismic refraction profiles off Lofoten, northern Norway / A. SellevollM.A. Goldschmidt-Rokita, H.B. Hirschleber, F. Avedik.
| Title: | Results of two seismic refraction profiles off Lofoten, northern Norway / A. SellevollM.A. Goldschmidt-Rokita, H.B. Hirschleber, F. Avedik. |
| Author(s): | Goldschmidt-Rokita, A. SellevollM.A. Hirschleber, H. B. Avedik, F. |
| Date: | 1988. |
| In: | Norges Geologiske Undersøkelse. Special Publication. (1988.), Vol. 3 (1988) |
| Abstract: | Deep sounding was used to study transition from continental to oceanic crustal structure along two profile lines. Results show that basalt flow covering major part of margin between Vøring Plateau Escarpment and shelf edge off Lofoten is underlain by thick sedimentary sequences. Very strong Moho reflections are observed, indicating abrupt change in Moho depth from 25 - 14 km (ocean) over less than 30 km. Data also suggest block-like crustal structure beneath islands. |
| Notes: | Norges Geologiske Undersøkelse. Special Publication. Vol. 3 :49-57 (1988). |
| Keywords: | 550.34 -- Seismology. 551.1/.4 -- Geology. 551.3.051 -- Sedimentation and stratification. 551.462 -- Submarine topography, bottom forms. 552.323.5 -- Basalt. B -- Geology and soil sciences. (*3) -- Arctic regions. (*58) -- Norway. |
| SPRI record no.: | 96403 |
LDR 01556naa#a2200000#a#4500 001 SPRI-96403 005 20230321122609.0 007 ta 008 230321s1988####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-96403 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aGoldschmidt-Rokita, A. SellevollM.A. 245 10 ‡aResults of two seismic refraction profiles off Lofoten, northern Norway /‡cA. SellevollM.A. Goldschmidt-Rokita, H.B. Hirschleber, F. Avedik. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1988. 300 ## ‡ap. 49-57 :‡bdiags., maps. 500 ## ‡aNorges Geologiske Undersøkelse. Special Publication. Vol. 3 :49-57 (1988). 520 3# ‡aDeep sounding was used to study transition from continental to oceanic crustal structure along two profile lines. Results show that basalt flow covering major part of margin between Vøring Plateau Escarpment and shelf edge off Lofoten is underlain by thick sedimentary sequences. Very strong Moho reflections are observed, indicating abrupt change in Moho depth from 25 - 14 km (ocean) over less than 30 km. Data also suggest block-like crustal structure beneath islands. 650 07 ‡a550.34 -- Seismology.‡2udc 650 07 ‡a551.1/.4 -- Geology.‡2udc 650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc 650 07 ‡a551.462 -- Submarine topography, bottom forms.‡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# ‡aHirschleber, H. B. 700 1# ‡aAvedik, F. 773 0# ‡7nnas ‡tNorges Geologiske Undersøkelse. Special Publication. ‡gVol. 3 (1988) ‡wSPRI-84344 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230321