Sr. Ogilvie et Pwj. Glover, The petrophysical properties of deformation bands in relation to their microstructure, EARTH PLAN, 193(1-2), 2001, pp. 129-142
Deformation bands are significant discontinuities in reservoir sandstones p
roviding baffles to the migration of fluids and acting as seats for hydroca
rbon accumulations. Their contribution to these processes is dependent upon
a range of inter-related factors including lateral continuity, relative di
splacement, reservoir geohistories and rock microstructure. Deformation ban
ds have millimetre-scale displacements, which are smaller than the seismic
resolution, and hence the study of their microstructure from reservoir core
s is a necessary tool in the prediction of their fault seal potential. The
latter is only achieved if detailed petrophysical measurements of fault mic
rostructure are carried out using techniques, which are suitable for measur
ement of very low permeability fault rock at the relevant scale. Convention
al techniques of fault rock porosity and permeability determination invite
host rock bias in measurement and inevitably underestimate the potential of
these structures as fluid barriers. Pressure decay probe permeametry used
in this study has the advantage of measuring small volumes of rock at Finer
spatial resolutions and detailed permeability distributions around common
types of deformation bands are obtained. Together with supporting data prov
ided by conventional core analysis techniques, these measurements show that
the greatest differences in petrophysical properties relative to host rock
occur in those bands, which have experienced cataclasis, These results pro
vide valuable input into reservoir simulation models and help reduce much o
f the uncertainty regarding the role of different types of deformation band
s in fault seal. (C) 2001 Elsevier Science B.V. All rights reserved.