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- W2067651771 abstract "On the continental shelf off Mid Norway at water depths ranging from 150 to 350 m, large areas of the seabed consist of plastic clays with a rugged surface topography and an amorphous (opaque) subsurface acoustic appearance. Five topographic (side-scan sonar) and shallow seismic examples are presented and discussed. Many of the mounds and ridges are suspected to be of a clay diapiric nature. Numerous gas seepages originating from opaque clays have also been found off Mid Norway. A tentative formation model for the ridges and dome-shaped features is proposed. The model is based on suspected differential gas charging of subsurface sediments and clay diapirism caused by differential clay buoyancy." @default.
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- W2067651771 date "1990-08-01" @default.
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- W2067651771 title "Suspected gas-associated clay diapirism on the seabed off Mid Norway" @default.
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- W2067651771 doi "https://doi.org/10.1016/0264-8172(90)90004-z" @default.
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