Transpression
Transpressional shear zones are characterized by the co-existence of different structures, related to both strike-slip shear and shortening. End member structures include pure strike-slip faults and pure thrust (reverse) faults. Faults which have components of both (termed 'oblique' slip faults) are abundant. In addition, structures such as folds, tension fractures and riedel shears all form in the shear zone but at different angles to those observed in simple strike-slip fault zones.
Restraining bend
Restraining bends are transpressional structures that form where the orientation of a strike-slip fault becomes oblique to the regional slip vector causing local compression or uplift [1] They also form where two segments of a strike-slip fault overlap, and the relay zone between the segments experiences transpression. Restraining bends often form positive flower structures or pop-up ridges.
Transpressional regions
- Altai Mountains (Western Mongolia and Southern Siberia, Russia)
- Western Aleutian Subduction Zone
- Gobi Altai (Central Mongolia)
- "Big Bend" of the San Andreas Fault Zone, (California, USA)
- Alpine Fault in New Zealand
Related links
- Transtension
- Structural Geology
- Strike-slip tectonics
References
- ↑ Christie-Blick, N. and Biddle, K.T. (1985). Deformation and basin formation along strike-slip faults in N. Christie-Blick and K.T. Biddle (eds.), Strike-Slip Deformation, Basin Formation and Sedimentation. SEPM Special Publications, 37.