Anisotropy of permeability in faulted porous sandstones

N. J. C. Farrell, D. Healy, C. W. Taylor

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Abstract

Studies of fault rock permeabilities advance the understanding of fluid migration patterns around faults and contribute to predictions of fault stability. In this study a new model is proposed combining brittle deformation structures formed during faulting, with fluid flow through pores. It assesses the impact of faulting on the permeability anisotropy of porous sandstone, hypothesising that the formation of fault related micro-scale deformation structures will alter the host rock porosity organisation and create new permeability pathways. Core plugs and thin sections were sampled around a normal fault and oriented with respect to the fault plane. Anisotropy of permeability was determined in three orientations to the fault plane at ambient and confining pressures. Results show that permeabilities measured parallel to fault dip were up to 10 times higher than along fault strike permeability. Analysis of corresponding thin sections shows elongate pores oriented at a low angle to the maximum principal palaeo-stress (σ1) and parallel to fault dip, indicating that permeability anisotropy is produced by grain scale deformation mechanisms associated with faulting. Using a soil mechanics ‘void cell model’ this study shows how elongate pores could be produced in faulted porous sandstone by compaction and reorganisation of grains through shearing and cataclasis.
Original languageEnglish
Pages (from-to)50-67
Number of pages18
JournalJournal of Structural Geology
Volume63
Early online date3 Mar 2014
DOIs
Publication statusPublished - Jun 2014

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anisotropy
sandstone
permeability
faulting
fault plane
thin section
dip
brittle deformation
soil mechanics
deformation mechanism
confining pressure
void
normal fault
host rock
fluid flow
compaction
porosity
fluid
prediction
rock

Keywords

  • permeability
  • anisotropy
  • faulting
  • porous sandstone
  • cataclasis
  • confining pressure

Cite this

Anisotropy of permeability in faulted porous sandstones. / Farrell, N. J. C.; Healy, D.; Taylor, C. W.

In: Journal of Structural Geology, Vol. 63, 06.2014, p. 50-67.

Research output: Contribution to journalArticle

Farrell, N. J. C. ; Healy, D. ; Taylor, C. W. / Anisotropy of permeability in faulted porous sandstones. In: Journal of Structural Geology. 2014 ; Vol. 63. pp. 50-67.
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