Brittle structures focused on subtle crustal heterogeneities: implications for flow in fractured rocks

A. M. Soden, Z. K. Shipton, R. J. Lunn, S. I. Pytharouli, J. D. Kirkpatrick, A. F. do Nascimento, F. H. R. Bezerra

Research output: Contribution to journalArticlepeer-review

18 Citations (Scopus)
184 Downloads (Pure)


Host rock mechanical heterogeneities influence the spatial distribution of deformation structures and hence, predictions of fault architecture and fluid flow. A critical factor, commonly overlooked, is how rock mechanical properties can vary over time, and how this will alter deformation processes and resultant structures. We present field data from an area in the Borborema Province, NE Brazil, that demonstrate how temporal changes in deformation conditions, and consequently processes, exerts a primary control on the spatial distribution and geometric attributes of evolving deformation structures. Further, each temporal deformation phase imparted different hydraulic architecture. The earliest flowing structures localized upon subtle ductile heterogeneities. Following fault formation, both fault core and damage zone were flow conduits. In later stages of faulting pseudotachylyte welding created a low-permeability fault core and annealed high-permeability fractures within the fault damage zone. Modern flow occurs along a zone of later open shear fractures, defined by the mechanical strength contrast between the host rock and annealed fault. This second hydraulically-conductive zone extends 100s of meters from the edge of the annealed fault damage zone, creating a flow zone far wider than would be predicted using traditional fault scaling relationships. Our results demonstrate the importance of understanding successive deformation events for predicting the temporal and spatial evolution of hydraulically active fractures.
Original languageEnglish
Pages (from-to)509-524
Number of pages16
JournalJournal of the Geological Society
Issue number4
Early online date28 Apr 2014
Publication statusPublished - Jul 2014


  • crustal structure
  • deformation
  • fault zone
  • heterogeneity
  • host rock
  • hydraulic conductivity
  • hydraulic fracture
  • pseudotachylite
  • rock mechanics
  • spatial distribution
  • temporal evolution


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