Anisotropic pore fabrics in faulted porous sandstones. (November 2017)

• Record Type: Journal Article
• Authors: Farrell, N.J.C.; Healy, D.
• Is Part Of: Journal of structural geology. Volume 104(2017:Nov.)
• Page Start: 125
• Page End: 141
• Publication Date: 2017-11
• Subjects: Porosity -- Faulting -- Image analysis -- Anisotropy -- Porous sandstone -- Permeability; Geology, Structural -- Periodicals; Géomorphologie structurale -- Périodiques; Geology, Structural; Periodicals; 551.805
• DOI: 10.1016/j.jsg.2017.09.010
• Languages: English
• ISSNs: 0191-8141

Abstract

Abstract: The fabric of pores in sedimentary rocks around fault zones can be subject to significant modification. Knowledge of how pore fabrics vary during and after faulting is important for understanding how rocks transmit fluids around fault zones, and can help to predict mechanical instability due to changes in pore fluid pressure. Datasets detailing the geometry of pore fabrics in faulted porous rocks are lacking. This paper describes pore fabrics quantified from two outcrops of normally faulted sandstone. The porosity and the size, shape and geometry of pores were quantified from core plugs and thin sections. Results were mapped within a framework of the faults to better illustrate how these datasets may be used to improve understanding of fluid flow around fault zones. Results from a mature, quartz-rich arenite show a change in pore fabric from pores oriented horizontally and parallel to laminations to pores oriented at a low angle to σ1 . Pore fabrics quantified from a clay-rich, quartz sub-arkose changed from moderate aspect ratio pores with no preferred orientation, to high aspect ratio pores oriented dominantly sub-parallel to the fault surface. Permeabilities measured on corresponding core plugs showed anisotropy of permeability with maximum permeability oriented down fault dip around both faults. Highlights: Anisotropic pore fabrics have been identified in faulted porous sandstones. Pores in unfaulted sandstones are oriented horizontal and parallel to laminations. Pores in faulted sandstones are oriented sub - parallel to the fault plane and/or sigma1. Anisotropic pores induce anisotropy of permeability in faulted rocks. Results from this study can be used to predict how fluids are transmitted around faults.