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Getting a feel for 3D geometry of seismic scale structure is not easy, in spite of advances in 3D visualisation and use of 3D seismic. The coastal sections in west Somerset provide a superb location to do just this in the field. Excellent cliff exposures and wave cut platforms allow geometries to be examined in 3D.

Several phases of deformation have affected the area and normal faults at a variety of scales can be studied, along with reverse and strike-slip movement, and the effects of basin inversion.

The course addresses:
  • geometry and style of seismic and smaller scale normal faults, predictive tools and methods for improving fault interpretation and mapping.
  • variation in footwall and hangingwall deformation, patterns of structural closure.
  • relationship between large and smaller scale structures, deformation at fault terminations.
  • fault and damage zone character.
  • reactivation of faults, comparison of rollover and inversion anticlines.
  • compression and strike-slip components of movement.

This course is highly recommended for anyone involved in seismic interpretation or building reservoir models.


Seismic scale fault

Closure against faults on the foreshore

small scale deformation in the footwall and hangingwall


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