Forward kinematic modeling of fault-bend folding. (February 2021)

• Record Type: Journal Article
• Authors: Connors, Christopher D.; Hughes, Amanda N.; Ball, Stephen M.
• Is Part Of: Journal of structural geology. Volume 143(2021)
• Publication Date: 2021-02
• Subjects: Fault-bend fold -- Kinematic model -- Rounded hinge -- Parallel fold -- Thrust sheet -- Balancing; Geology, Structural -- Periodicals; Géomorphologie structurale -- Périodiques; Geology, Structural; Periodicals; 551.805
• DOI: 10.1016/j.jsg.2020.104252
• Languages: English
• ISSNs: 0191-8141

Abstract

Abstract: We present a forward numerical modeling approach for fault-bend folding based on a velocity description of deformation. The approach incorporates algorithms capable of modeling multiple fault bends of different geometries (e. g. fault bends not stepping up from a detachment), imbricates, and variable velocity-boundary orientations, with corresponding varying slip ratios. When modeling contraction, the approach is capable of reproducing rounded-hinges and parallel folds with localized bed thinning or thickening commonly observed in natural structures. Extensional fault-bend folds can be modeled using the same set of equations, with the minor modification that velocity boundary orientations are defined independently of the fault shape. The modeled structures conserve area, and commonly observed features of extensional fault-bend folds, such as rollover structures with growth, are produced. Thus, we present a unified inclined-shear and flexural-slip general transformation associated with displacement over bends in faults, describing the theoretical framework which we have implemented in the associated program, fbfFor. We show the utility of this kinematic approach by matching seismic reflection examples, analog models, and mechanical models of fault-bend folds to create progressive, balanced kinematic interpretations and gain further insight into the formation of these structures. Highlights: Parallel fault-bend folds with rounded hinges modeled. Heterogeneous layer-parallel strain in cross sections. Inclined shear and flexural slip unified into general transformation. Kinematic models match seismic, analog and mechanical models.