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- W2061857013 abstract "Seismic experiments conducted on ice stream B, part of the marine ice sheet of West Antarctica, show a meters‐thick layer immediately beneath the 1000‐m‐thick ice. A seismic experiment consisting of wide‐angle reflection profiling along a line parallel to ice stream flow was conducted to determine the properties of this layer. Inversion of seismic travel times yields a compressional wave speed of less than 1700 m s −1 and a shear wave speed less than 160 m s −1 for the layer. These very low wave speeds imply that the material in the layer is highly porous and is saturated with water at a high pore pressure. Based on wave speeds in other saturated, unconsolidated sediments, we believe that a porosity substantially greater than 0.32, probably around 0.4, and an excess of overburden pressure over pore pressure of only 50 kPa (0.5 bar) characterize the layer at this location." @default.
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- W2061857013 date "1987-08-10" @default.
- W2061857013 modified "2023-10-16" @default.
- W2061857013 title "Till beneath ice stream B: 1. Properties derived from seismic travel times" @default.
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- W2061857013 doi "https://doi.org/10.1029/jb092ib09p08903" @default.
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