191 D40. Structural Geology and Tectonics: Advances in Understanding Fault Systems, Plate Boundaries and Deformation: Observations and Experiments

Tuesday, 24 October 2017
8:00 AM - 12:00 PM
Tahoma 3

DEVELOPMENT OF NON-STEADY STATE SLIP PARTITIONING UNDER OBLIQUE CONVERGENCE

Paper number: 191-13
Program: Technical Sessions
Time: 10:50 AM – 11:10 AM

Authors

Abstract

Oblique convergence experiments in wet kaolin develop slip-partitioned fault systems rather than developing a single active oblique-slip fault. The development of two fault surfaces, which consumes greater work than a single fault, arises due to the changes in the local stress state after development of the first fault. As one strain component is relieved by either the early strike-slip along a pre-existing weakness or oblique slip along a newly created reverse fault, the local stress field then favors development of the other fault type.

The suite of experiments in this study reveal three styles of slip partitioning development controlled by the convergence angle and presence of a pre-existing crustal weakness. The first style (Type 1) observed in the low convergent angle experiments (5°) grow strike-slip faults prior to reverse faults regardless of whether the fault is precut or not. This result suggests that the presence of a pre-existing weakness has a lesser effect on the development of slip partitioning in strike-slip dominated systems than for more moderate angle convergent margins. For the more moderate convergence angle experiments (10°, 15°, 20° precut and uncut), the sequence of slip partitioning is dominantly controlled by the presence of a pre-existing crustal weakness. In all experiments, the primarily reverse fault forms first. Subsequent slip partitioning develops either with the initiation of strike-slip along the precut fault (Type 2) or growth of a secondary reverse fault where the first fault is steepest. Subsequently, this slip on the first fault transitions to strike-slip (Type 3). Here, the relative angle of convergence seems to play a subordinate role, controlling the timing of slip partitioning development (higher convergence angles partitioning earlier) but not the sequence of faulting leading up to slip partitioning.

Non steady-state slip rates along the strike-slip and reverse faults for both precut and uncut experiments suggest that faults in slip-partitioned systems continuously adjust to the conditions produced by deformation along the other faults. The non steady-state behavior is manifest as temporally oscillating relative rates of slip between strike-slip and reverse faulting due the redistribution of shear and convergent strain as the fault system develops.

Geological Society of America Abstracts with Programs. Vol. 49, No. 6

doi: 10.1130/abs/2017AM-302445

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