Recurrent Pleistocene mega-failures on the SW Barents Sea margin
Submarine slides have been instrumental in shaping the Late Neogene NE Atlantic continental margin. We document a margin setting north of 70°N capable of generating recurrent huge Pleistocene mass-movements. The 1.0–0.2 Ma old Bjørnøya Fan Slide Complex includes three buried mega-slides, which have...
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| Published in: | Earth and planetary science letters Vol. 258; no. 3; pp. 605 - 618 |
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| Main Authors: | , , |
| Format: | Journal Article |
| Language: | English |
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Elsevier B.V
30-06-2007
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| Abstract | Submarine slides have been instrumental in shaping the Late Neogene NE Atlantic continental margin. We document a margin setting north of 70°N capable of generating recurrent huge Pleistocene mass-movements. The 1.0–0.2 Ma old Bjørnøya Fan Slide Complex includes three buried mega-slides, which have left scars containing up to 500 m-thick debris units. The two largest slides may have had a retrogressive development, cover areas of the order of ∼
120
×
10
3 km
2, and involved ∼
25
×
10
3 km
3 of sediments. Thus, the failures involved an order of magnitude more sediment than the Storegga Slide, the world's largest exposed slide. The mega-slides occurred during the Northern Hemisphere Glaciations, characterized by greatly enhanced deposition rates leading to the construction of the 3-km-thick Bjørnøya Trough Mouth Fan that progressively loaded a softer Miocene–Oligocene substratum. This setting induced excess pore pressure and sediment instability, conditions favorable for sliding. External trigger mechanisms, such as earthquakes, may have facilitated the mass-wasting process. |
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| AbstractList | Submarine slides have been instrumental in shaping the Late Neogene NE Atlantic continental margin. We document a margin setting north of 70 super(o)N capable of generating recurrent huge Pleistocene mass-movements. The 1.0-0.2 Ma old Bjornoya Fan Slide Complex includes three buried mega-slides, which have left scars containing up to 500 m-thick debris units. The two largest slides may have had a retrogressive development, cover areas of the order of ~120x10 super(3) km super(2), and involved ~25x10 super(3) km super(3) of sediments. Thus, the failures involved an order of magnitude more sediment than the Storegga Slide, the world's largest exposed slide. The mega-slides occurred during the Northern Hemisphere Glaciations, characterized by greatly enhanced deposition rates leading to the construction of the 3-km-thick Bjornoya Trough Mouth Fan that progressively loaded a softer Miocene-Oligocene substratum. This setting induced excess pore pressure and sediment instability, conditions favorable for sliding. External trigger mechanisms, such as earthquakes, may have facilitated the mass-wasting process. Submarine slides have been instrumental in shaping the Late Neogene NE Atlantic continental margin. We document a margin setting north of 70°N capable of generating recurrent huge Pleistocene mass-movements. The 1.0–0.2 Ma old Bjørnøya Fan Slide Complex includes three buried mega-slides, which have left scars containing up to 500 m-thick debris units. The two largest slides may have had a retrogressive development, cover areas of the order of ∼ 120 × 10 3 km 2, and involved ∼ 25 × 10 3 km 3 of sediments. Thus, the failures involved an order of magnitude more sediment than the Storegga Slide, the world's largest exposed slide. The mega-slides occurred during the Northern Hemisphere Glaciations, characterized by greatly enhanced deposition rates leading to the construction of the 3-km-thick Bjørnøya Trough Mouth Fan that progressively loaded a softer Miocene–Oligocene substratum. This setting induced excess pore pressure and sediment instability, conditions favorable for sliding. External trigger mechanisms, such as earthquakes, may have facilitated the mass-wasting process. |
| Author | Eldholm, Olav Faleide, Jan Inge Hjelstuen, Berit Oline |
| Author_xml | – sequence: 1 givenname: Berit Oline surname: Hjelstuen fullname: Hjelstuen, Berit Oline email: berit.hjelstuen@geo.uib.no organization: Department of Earth Science, University of Bergen, Allegt 41, N-5007 Bergen, Norway – sequence: 2 givenname: Olav surname: Eldholm fullname: Eldholm, Olav organization: Department of Earth Science, University of Bergen, Allegt 41, N-5007 Bergen, Norway – sequence: 3 givenname: Jan Inge surname: Faleide fullname: Faleide, Jan Inge organization: Department of Geosciences, University of Oslo, P.O.Box 1047 Blindern, N-0316 Oslo, Norway |
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| Snippet | Submarine slides have been instrumental in shaping the Late Neogene NE Atlantic continental margin. We document a margin setting north of 70°N capable of... Submarine slides have been instrumental in shaping the Late Neogene NE Atlantic continental margin. We document a margin setting north of 70 super(o)N capable... |
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| Title | Recurrent Pleistocene mega-failures on the SW Barents Sea margin |
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