On the origin and flow behavior of submarine slides on deep-sea fans along the Norwegian–Barents Sea continental margin

被引：1

作者：

A. Elverhøi

H. Norem

E. S. Andersen

J. A. Dowdeswell

I. Fossen

H. Haflidason

N. H. Kenyon

J. S. Laberg

E. L. King

H. P. Sejrup

A. Solheim

T. Vorren

机构：

[1] Department of Geology,

[2] Box 1047,undefined

[3] University of Oslo,undefined

[4] Blindern,undefined

[5] 0316 Oslo,undefined

[6] Norway,undefined

[7] Norwegian Geotechnical Institute,undefined

[8] Box 3930 Ullevaal Hageby,undefined

[9] 0806 Oslo,undefined

[10] Norway Present address: Dr. Ing Harald Norem Ltd. Fuglsetbakken 41,undefined

[11] 6400 Molde,undefined

[12] Norway,undefined

[13] Centre for Glaciology,undefined

[14] Institute of Earth Studies,undefined

[15] University of Wales,undefined

[16] Aberystwyth,undefined

[17] Dyfed SY23 3DB Wales,undefined

[18] UK,undefined

[19] Department of Geology,undefined

[20] University of Bergen,undefined

[21] Allegt.41,undefined

[22] N-5007 Bergen,undefined

[23] Norway,undefined

[24] Southampton Oceanography Centre,undefined

[25] Empress Dock,undefined

[26] Southampton,undefined

[27] SO14 3ZH,undefined

[28] UK,undefined

[29] Institute of Biology and Geology,undefined

[30] University of Tromsø,undefined

[31] N-9037,undefined

[32] Tromsø,undefined

[33] Norway,undefined

[34] Norwegian Polar Institute,undefined

[35] P.O. Box 5072 Majorstua,undefined

[36] N-0301 Oslo,undefined

[37] Norway,undefined

来源：

Geo-Marine Letters | 1997年 / 17卷

关键词：

Sedimentation; Flow Model; Characteristic Length; Flow Behavior; Continental Margin;

D O I：

暂无

中图分类号：

学科分类号：

摘要：

Debris lobes with characteristic lengths, widths, and thickness of 30–200 km, 2–10 km, and 10–50 m, respectively, represent the main building blocks of deep-sea fans along the Norwegian–Barents Sea continental margin. Their formation is closely related to the input of clay-rich sediments to the upper continental slope by glaciers during periods of maximum ice advance. It is likely that slide release was a consequence of an instability arising from high sedimentation rates on the upper continental slope. The flow behavior of the debris lobes can be described by a Bingham flow model.

引用

页码：119 / 125

页数：6

共 50 条

[41] Evolution of shelf-margin clinoforms and deep-water fans during the middle Eocene in the Sorvestsnaget Basin, southwest Barents Sea
Safronova, Polina A.
Henriksen, Sverre
Andreassen, Karin
Laberg, Jan Sverre
Vorren, Tore O.
AAPG BULLETIN, 2014, 98 (03) : 515 - 544
[42] DEEP GEOTHERMAL STRUCTURE AND MANTLE HEAT-FLOW ALONG THE BARENTS SEA EAST ALPS GEOTRAVERSE
MILANOVSKY, SY
TECTONOPHYSICS, 1984, 103 (1-4) : 175 - 192
[43] Deep-water scleractinian corals promote higher biodiversity in deep-sea meiofaunal assemblages along continental margins
Bongiorni, L.
Mea, M.
Gambi, C.
Pusceddu, A.
Taviani, M.
Danovaro, R.
BIOLOGICAL CONSERVATION, 2010, 143 (07) : 1687 - 1700
[44] Chemical characterization of deep-sea corals from the continental slope of Santos Basin (southeastern Brazilian upper margin)
Trevizani, Tailisi Hoppe
Nagai, Renata Hanae
Lopes Figueira, Rubens Cesar
Gomes Sumida, Paulo Yukio
de Mahiques, Michel Michaelovitch
OCEAN AND COASTAL RESEARCH, 2022, 70
[45] Controlling Parameters of Benthic Deep-Sea Foraminiferal Biogeography at the Brazilian Continental Margin (11-22°S)
Saupe, Anna
Schmidt, Johanna
Petersen, Jassin
Bahr, Andre
Dias, Bruna Borba
Albuquerque, Ana Luiza Spadano
Diaz Ramos, Rut Amelia
Grunert, Patrick
FRONTIERS IN MARINE SCIENCE, 2022, 9
[46] THE CYCLING AND ACCUMULATION OF BIOGENIC SILICA AND ORGANIC-CARBON IN ANTARCTIC DEEP-SEA AND CONTINENTAL-MARGIN ENVIRONMENTS
DEMASTER, DJ
NELSON, TM
HARDEN, SL
NITTROUER, CA
MARINE CHEMISTRY, 1991, 35 (1-4) : 489 - 502
[47] Postglacial (after 18ka) deep-sea sedimentation along the Hikurangi subduction margin (New Zealand): Characterisation, timing and origin of turbidites
Pouderoux, Hugo
Proust, Jean-Noël
Lamarche, Geoffroy
Orpin, Alan
Neil, Helen
Marine Geology, 2012, 295-298 : 51 - 76
[48] DEEP-SEA DRILLING PROJECT HEAT-FLOW AND MODELS OF THE RIFTED WEST ROCKALL MARGIN
HYNDMAN, RD
ROBERTS, DG
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1987, 92 (B9): : 9376 - 9384
[49] Flow Behavior of Aqueous Solution of Exopolysaccharide Secreted by a Deep-sea Mesophilic Bacterium
Li Hai-Ping
Liu Sheng-Bo
Hou Wan-Guo
CHEMICAL JOURNAL OF CHINESE UNIVERSITIES-CHINESE, 2012, 33 (05): : 1025 - 1030
[50] Modern submarine canyon feeder-system and deep-sea fan growth in a tectonically active margin (northern Sicily)
Gamberi, Fabiano
Rovere, Marzia
Marani, Michael P.
Dykstra, Mason
GEOSPHERE, 2015, 11 (02): : 307 - 319

← 1 2 3 4 5 →