EGU25-11403, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-11403
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Thursday, 01 May, 14:05–14:15 (CEST)
 
Room G2
Fault characteristics from outcrop and reflection seismic studies
Anita Torabi
Anita Torabi
  • University of Oslo, Geosciences, Oslo, Norway (anita.torabi@geo.uio.no)

Faults can be studied at different scales and through different methods. Hence, every method provides some insight into our understanding of fault geometry and properties despite the limitations inherent to these methods. Among fault characteristics, fault geometric attributes such as fault plane roughness, displacement, length, and width can be studied using both outcrops and 3D reflection seismic data. Fault geometric attributes from different scales of study are then used within fault scaling laws to increase our knowledge of fault growth mechanism and mechanics.  In addition, fault rock properties from fault core and damage zone allow us to study the effect of faults on the fluid flow behavior of rocks as well as their mechanical integrity. In order to have a better knowledge of fault characteristics and mechanical behavior, it is important to integrate fault geometric studies with fault rock properties.  This needs an interdisciplinary approach, combining geomechanics, earthquake and exploration seismology with structural geology, hence, allowing us to study both active and non-active faults from different perspectives.

How to cite: Torabi, A.: Fault characteristics from outcrop and reflection seismic studies, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-11403, https://doi.org/10.5194/egusphere-egu25-11403, 2025.