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Junhua Guo, Michael B. Underwood, William J. Likos and Demian M. Saffer Apparent overconsolidation of mudstones in the Kumano Basin of southwest Japan: Implications for fluid pressure and fluid flow within a forearc setting Geochemistry, Geophysics, Geosystems 14

Version of Record online: 25 APR 2013 | DOI: 10.1029/2012GC004204

Key Points

  • Values of preconsolidation pressure indicate overconsolidation.
  • Drainage through landward-dipping turbidites leads to hydrostatic pore pressure.
  • Cementation in the lower basin is responsible for apparent overconsolidation.

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