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- W2085752007 abstract "The South Australian Basin has been the site of extensive Antarctic Bottom Water (AABW) scour during the late Cenozoic. The combination of detailed stratigraphy and sedimentological analyses of three piston cores allowed the identification of the major episodes of high bottom-current paleovelocity. The chronology of the cores was determined by magnetostratigraphy and biostratigraphy. Five parameters, mean, mode, skewness, coarsest 1%, and sorting of the carbonate-free silt particle size distribution were used to infer periods of high paleovelocity. Sorting was found to be an insensitive parameter within the inferred paleovelocity regimes. The two major high-velocity episodes during the last 3.3 m.y. occurred during the Gauss Chron and the upper Matuyama Chron. Several short episodes of high bottom-water velocity occurred during the Matuyama Chron. Only one minor pulse was identified during the Brunhes Chron (0–0.73 m.y.B.P.). The high velocity episode during the Gauss Chron produced a disconformity separating Miocene and middle Pliocene sediments while the upper Matuyama episode may be responsible for the widespread disconformity at or near the seafloor which has been identified in many cores in the region." @default.
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- W2085752007 date "1982-03-01" @default.
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- W2085752007 title "Timing of bottom-water scour recorded by sedimentological parameters in the South Australian Basin" @default.
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- W2085752007 doi "https://doi.org/10.1016/0025-3227(82)90155-4" @default.
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