GSA Annual Meeting in Denver, Colorado, USA - 2016

Paper No. 265-39
Presentation Time: 9:00 AM-6:30 PM


NABAVI, Seyed Tohid1, ALAVI, Seyed Ahmad1, MOHAMMADI, Soheil2, GHASSEMI, Mohammad Reza3 and SHIRZAEI, Manoochehr4, (1)Faculty of Earth Sciences, Department of Geology, Shahid Beheshti University, Iran, Tehran, Velenjak, Shahriari Sq., Daneshjoo Blv., Tehran, 1983969411, Iran (Islamic Republic of), (2)High Performance Computing Laboratory, School of Civil Engineering, University of Tehran, Iran, Tehran, Enghelab Sq. Enghelab St., Tehran, 4563-11155, Iran (Islamic Republic of), (3)Research Institute for Earth Sciences, Geological Survey of Iran, Iran, Tehran, Azadi Sq., Meraj Blv., Tehran, 1494-13185, Iran (Islamic Republic of), (4)School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287,

Two-dimensional finite-element modelling, using a commercial FEM software, ABAQUS, is used to compute stress distribution and strain localization patterns in a transpression zone between two pre-existing right-stepping, left-lateral strike-slip fault segments as a function of the orientation of the applied far-field compressive stress. Linear elastic rheology and plane strain conditions are assumed. Regional compression is applied at different convergence angles relative to the fault strike. Three representative fault segment interactions are modelled: underlapping, neutral and overlapping. The numerical results indicate that at the onset of deformation, displacement vectors are oblique to the regional compression direction. The orientations of the local σ1 and σ3 strongly depends on structural position within the transpression zone. In low-σ3 zones, which occur close to fault tips, wing cracks and horsetail arrays would propagate outwards along a curvilinear path. For neutral and overlapping fault steps, there is a contractional linking damage zone, mostly crosscutting P-shears, between the fault segments. For overlapping faults, the σ1 direction within the transpression zone is highly deflected and forms a sigmoidal pattern, which is created by two rotational flow patterns close to the fault tips. These flow patterns are related to friction effects and different shear deformation, from pure shear outside of the fault steps toward simple shear along the fault segments. Interaction between the two fault segments perturbs stress field and reflects the heterogeneous nature of deformation. A lozenge- (for underlapping steps), rhomboidal- (for neutral steps) and sigmoidal-shaped (for overlapping steps) transpression zone is bounded by curved, oblique-slip reverse faults that cause block rotation between the two segments. The modelled mean stress pattern shows a similar pattern to that of the contractional steps, and decrease and increase in underlapping and overlapping fault steps, respectively. Comparison of the Kuh-e-Hori transpression zone, a doubly plunging asymmetric anticlinal structure, between the Esmail-abad and West Neh left-stepping right-lateral strike-slip fault segments in SE Iran with the modelling results shows strong similarities with the neutral step configuration.