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Seismic images and drilling tell the story of fluids in a plate-boundary fault

Authors

  • ODP Leg 156 Shipboard Science Party


Abstract

How do polarity and amplitude variations of seismic images relate to variations in fluid pressure, permeability, and other sediment physical properties? If these questions can be answered, seismic data can be used as a predictor of fluid properties in fault zones. Once applied, these data can be used to study earthquake hazards and hydrocarbon and groundwater migration. Shallowly dipping decollement faults (detachments thrusts) beneath accretionary prisms formed at convergent margins are ideal locations for calibrating seismic reflection images as proxies for fluid processes [Shipley etal, 1994] (Figure 1).

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