World's largest extrusive body of sand?

被引:24
作者
Loseth, Helge [1 ]
Rodrigues, Nuno [1 ]
Cobbold, Peter R. [2 ,3 ]
机构
[1] Statoil Res Ctr, NO-7005 Trondheim, Norway
[2] Univ Rennes 1, Geosci Rennes UMR6118, F-35042 Rennes, France
[3] CNRS, F-35042 Rennes, France
关键词
NORTHERN NORTH-SEA; SANDSTONE INTRUSIONS; COMPACTION;
D O I
10.1130/G33117.1
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Using three-dimensional seismic and well data from the northern North Sea, we describe a large (10 km(3)) body of sand and interpret it as extrusive. To our knowledge, this is the world's largest such sandbody. It would bury Manhattan, New York (60 km(2)), under 160 m of sand, or the whole of London, UK (1579 km(2)), under 6 m of sand. This sand vented to the seafloor, when it was more than 500 m deep, during the Pleistocene glacial period. The sandbody (1) covers an area of more than 260 km(2), (2) is up to 125 m thick, (3) fills low areas around mounds, which formed when underlying sand injectites lifted the overburden, (4) wedges out, away from a central thick zone, (5) is locally absent along irregular ditches, 20 km long and up to 50 m deep, which overlie feeders on the flanks of the mounds, and (6) consists of fine-grained to medium-grained, sub-rounded to rounded grains. We compare the distribution of the sand with the results of scaled physical experiments. In our interpretation, high fluid pressure fractured the regional Hordaland Group seal in the study area, so that fluidized sand moved rapidly to the seafloor through fissures on the flanks of underlying mounds, mixed with seawater, and formed lateral gravity currents. These transported the sand as much as 8 km away from the blow-out fissures and formed extruded sand sheets. Large extrusive sands represent a new type of economically interesting reservoir.
引用
收藏
页码:467 / 470
页数:4
相关论文
共 21 条
[1]   The geometry and emplacement of conical sandstone intrusions [J].
Cartwright, Joe ;
James, David ;
Huuse, Mads ;
Vetel, William ;
Hurst, Andrew .
JOURNAL OF STRUCTURAL GEOLOGY, 2008, 30 (07) :854-867
[2]  
Eidvin T, 2001, NORSK GEOL TIDSSKR, V81, P119
[3]   Use of vegetable oil and silica powder for scale modelling of magmatic intrusion in a deforming brittle crust [J].
Galland, O ;
Cobbold, PR ;
Hallot, E ;
d'Ars, JD ;
Delavaud, G .
EARTH AND PLANETARY SCIENCE LETTERS, 2006, 243 (3-4) :786-804
[4]   On steady homogeneous sand-water flows in a vertical conduit [J].
Gallo, F ;
Woods, AW .
SEDIMENTOLOGY, 2004, 51 (02) :195-210
[5]  
HURST A., 2007, AAPG MEMOIRS, V87
[6]   Extrusive sandstones (extrudites): a new class of stratigraphic trap? [J].
Hurst, Andrew ;
Cartwright, Joseph A. ;
Huuse, Mads ;
Duranti, Davide .
DELIBERATE SEARCH FOR THE STRATIGRAPHIC TRAP, 2006, 254 :289-+
[7]   Physical characteristics of sand injectites [J].
Hurst, Andrew ;
Scott, Anthony ;
Vigorito, Mario .
EARTH-SCIENCE REVIEWS, 2011, 106 (3-4) :215-246
[8]   Eocene sandstone intrusions in the Tampen Spur area (Norwegian North Sea Quad 34) imaged by 3D seismic data [J].
Huuse, M ;
Mickelson, M .
MARINE AND PETROLEUM GEOLOGY, 2004, 21 (02) :141-155
[9]  
Isaksen D., 1989, NPD-Bulletin, V5
[10]   Pre-Weichselian Quaternary glaciations of the British Isles, The Netherlands, Norway and adjacent marine areas south of 68°N: implications for long-term ice sheet development in northern Europe [J].
Lee, Jonathan R. ;
Busschers, Freek S. ;
Sejrup, Hans Petter .
QUATERNARY SCIENCE REVIEWS, 2012, 44 :213-228