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- W1985380853 abstract "Rapid sedimentation by fine-grained sediments on the upper slope of the New Jersey margin has generated nearly lithostatic fluid pressures. We use measured porosity from ODP Site 1073 to predict the in situ fluid pressures. We then simulate the pressure history with one-dimensional and two-dimensional sedimentation-compaction models. Two-dimensional models simulate a compaction-driven flow field that is dominated by lateral flow. This flow field increases overpressure and lowers effective stress on the lower slope. The combination of observation and theory provide a model that illuminates a mechanism through which seeps form and slope failure may occur in any rapidly loaded continental margin." @default.
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- W1985380853 date "2000-06-01" @default.
- W1985380853 modified "2023-09-26" @default.
- W1985380853 title "The New Jersey margin: compaction and fluid flow" @default.
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- W1985380853 doi "https://doi.org/10.1016/s0375-6742(00)00058-3" @default.
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