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Record #203044:
- #203044
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MARC recordMorphology of a non-glacigenic debris flow lobe in the Helland Hansen area investigated with 3D seismic data / A. Nygård, H. Haflidason, H.P. Sejrup.
| Title: | Morphology of a non-glacigenic debris flow lobe in the Helland Hansen area investigated with 3D seismic data / A. Nygård, H. Haflidason, H.P. Sejrup. |
| Author(s): | Nygård, A. Haflidason, H. Sejrup, H. P. |
| Date: | 2003. |
| Publisher: | Berlin: Springer |
| In: | European margin sediment dynamics : side-scan sonar and seismic images. (2003.), |
| Abstract: | Examines well-developed debris flow lobe on mid-Norwegian continental slope in Helland Hansen area. Lobe lies stratigraphically above acoustically layered hemiplagic sediments and below acoustically transparent package of glacigenic material, presumably debris flow material. Characteristic features distinguish this debris flows from those of glacigenic origin, suggesting this is "conventional" debris flow. |
| Notes: | In: European margin sediment dynamics : side-scan sonar and seismic images / Jürgen Mienert, Philip Weaver, eds. |
| Keywords: | 551.1/.4(26) -- Marine geology. 551.352/.353 -- Marine sediments, deep sea. 551.462.33 -- Continental slopes. 550.8 -- Geology and geophysics, applied. 550.834 -- Seismic survey methods. B -- Geology and soil sciences. (*3) -- Arctic regions. (*61) -- North Atlantic Ocean. |
| SPRI record no.: | 203044 |
LDR 01645naa#a2200000#a#4500 001 SPRI-203044 005 20240419065953.0 007 ta 008 240419s2003####gw#ab##|#####|0||#0#eng#d 035 ## ‡aSPRI-203044 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aNygård, A. 245 10 ‡aMorphology of a non-glacigenic debris flow lobe in the Helland Hansen area investigated with 3D seismic data /‡cA. Nygård, H. Haflidason, H.P. Sejrup. 260 ## ‡aBerlin :‡bSpringer,‡c2003. 300 ## ‡ap. 63-65 :‡bill., map. 500 ## ‡aIn: European margin sediment dynamics : side-scan sonar and seismic images / Jürgen Mienert, Philip Weaver, eds. 520 3# ‡aExamines well-developed debris flow lobe on mid-Norwegian continental slope in Helland Hansen area. Lobe lies stratigraphically above acoustically layered hemiplagic sediments and below acoustically transparent package of glacigenic material, presumably debris flow material. Characteristic features distinguish this debris flows from those of glacigenic origin, suggesting this is "conventional" debris flow. 650 07 ‡a551.1/.4(26) -- Marine geology.‡2udc 650 07 ‡a551.352/.353 -- Marine sediments, deep sea.‡2udc 650 07 ‡a551.462.33 -- Continental slopes.‡2udc 650 07 ‡a550.8 -- Geology and geophysics, applied.‡2udc 650 07 ‡a550.834 -- Seismic survey methods.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*61) -- North Atlantic Ocean.‡2udc 700 1# ‡aHaflidason, H. 700 1# ‡aSejrup, H. P. 773 0# ‡7nnam ‡aJürgen Mienert, Philip Weaver, eds. ‡tEuropean margin sediment dynamics : side-scan sonar and seismic images. ‡dBerlin : Springer, 2003. ‡wSPRI-201907 916 ## ‡aJW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419 ‡bJW