A wrench fault, also known as strike-slip fault, is a type of fault where the movement of blocks is primarily horizontal and is parallel to the strike of the fault plane. These can be either :
- Right lateral (dextral) : Where the opposite side moves to the right.
- Left lateral (sinistral) : Where the opposite side moves to the left.
These faults often form in transform plate boundaries or in strike-slip tectonic regimes and can be associated with complex geological structures like flower structures or pull-apart basins.
Importance in the Hydrocarbon Industry
- Trap formation :
- Pull-Apart Basins : Wrench faults can create pull-apart basins where sedimentary sequences accumulate. These basins can act as hydrocarbon kitchens due to rapid burial and heat flow.
- Releasing and Restraining Bends :
- Releasing bends may form basins and traps.
- Restraining bends can create uplift and anticlines that act as structural traps.
- Migration Pathways :
- Strike-slip faults can act as conuits for hydrocarbon migration.
- Fractures and fault planes may provide permeable pathways for hydrocarbons to move from source rocks to reservoirs.
- Compartmentalization :
- Wrench faults can segment reservoirs into compartments, which may –
- require multiple wells for full drainage.
- Affect pressure regimes across the fault zones.
- Wrench faults can segment reservoirs into compartments, which may –
- Reservoir Enhancement :
- In some cases, faulting can incrase permeability through fracturing.
- Enhanced secondary porosity due to movement and stress along the fault can improve reservoir quality.
- Seismic Interpretation and Risk :
- Wrench fault systems often have complex subsurface geometries, making them challenging but rewarding exploraiton targets.
- Understanding their orientation and offsert is key in 3D seismic interpretation and well planning.
Examples of Wrench fault related Plays
- San Andreas Fault (USA)
- North Sea
- Dead Sea Transform Fault