How Does the Orientation of a Preexisting Basement Weakness Influence Fault Development During Renewed Rifting? Insights From Three‐Dimensional Discrete Element Modeling. Issue 7 (27th July 2018)

• Record Type: Journal Article
• Authors: Deng, Chao; Gawthorpe, Robert L.; Fossen, Haakon; Finch, Emma
• Is Part Of: Tectonics. Volume 37:Issue 7(2018)
• Page Start: 2221
• Page End: 2242
• Publication Date: 2018-07-27
• Subjects: multiphase rifting -- fault reactivation -- fault segmentation -- fault growth -- fault interaction; Geology, Structural -- Periodicals; 551.8
• DOI: 10.1029/2017TC004776
• Languages: English
• ISSNs: 0278-7407

Abstract

Abstract: The variety in fault geometry, fault interaction style, and evolution of the fault network above a weak planar preexisting fault as a result of a change in the strike angle ( α ) of the preexisting fault relative to the extension direction is investigated using three‐dimensional discrete element modeling. The preexisting fault shows three reactivation modes: (i) full reactivation ( α ≥ 60°), (ii) partial reactivation ( α = 45°), and (iii) little or no reactivation ( α = 30°). A fully reactivated fault decreases the density, affects the orientation, and enhances the length and displacement of adjacent new faults. A partially reactivated fault generates some isolated fault segments along strike and also influences fault orientation. However, when the preexisting fault is not reactivated, its presence has little effect on the growth of new faults. Our study confirms that the reactivation pattern of a preexisting fault and its influence on new fault growth varies with its strike angle relative to the extension direction. It also demonstrates how a preexisting fault influences adjacent fault geometry and the fault network by changing the density, orientation, length, and displacement of newly formed faults. The work impacts understanding three‐dimensional fault geometries, the distribution, and evolution of fault networks in rift basins affected by preexisting faults and on predicting the extension direction of renewed rifting. Key Points: A preexisting fault is reactivated in three modes: full, partial, or none, due to its strike angle to the extension direction A reactivated preexisting fault influences the density, orientation, length, and displacement of adjacent newly formed faults Fault interaction styles vary with respect to the reactivation mode of preexisting faults