The Australian Geologist - Geological Society of Australia
The Australian Geologist - Geological Society of Australia
The Australian Geologist - Geological Society of Australia
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Book Reviews<br />
High-Strain Zones: structure<br />
and physical properties<br />
D Bruhn and L Burlini (Eds)<br />
2005<br />
<strong>Geological</strong> <strong>Society</strong> <strong>of</strong> London<br />
Special Publication 245<br />
Pages ISBN<br />
£95<br />
www.geolsoc.org.uk<br />
This book contains several paper presented at<br />
a special session on High Strain Zones at the<br />
EGS–AGU–EUG meeting in 2003 in Nice,<br />
France. It starts with an excellent review <strong>of</strong><br />
strain s<strong>of</strong>tening mechanisms identified over<br />
20 years ago and considers these in the light<br />
<strong>of</strong> more recent results arising from the application<br />
<strong>of</strong> new novel laboratory deformation<br />
techniques such as high strain in torsion<br />
experiments. It is clear from my own field<br />
studies that the Earth’s lithosphere is<br />
deformed by localised, narrow high strain<br />
zones on a range <strong>of</strong> scales from regional to<br />
outcrop. Recent studies by myself and my<br />
excellent honours students reveal parts <strong>of</strong><br />
the Wyangala Granite are transected by discontinuous<br />
high strain zones <strong>of</strong> hundreds <strong>of</strong><br />
metres width and kilometres length <strong>of</strong>ten<br />
near lithological (and hence rheologically<br />
important) boundaries. <strong>The</strong> localization <strong>of</strong><br />
deformation in high strain zones appears to<br />
be a universal property <strong>of</strong> rocks.<br />
This volume consists <strong>of</strong> 22 well-edited<br />
papers, which are clearly illustrated and<br />
beautifully bound to the very high standard.<br />
<strong>The</strong> papers can be divided into six main<br />
groups, although there is some overlap. In<br />
the first group there are six papers on field<br />
studies <strong>of</strong> high strain zone (HSZ) including<br />
the relationship between deformation and<br />
metamorphism. In the second group there<br />
are five papers on the physical properties <strong>of</strong><br />
HSZ in the field and laboratory. In the third<br />
group there are five papers on the rheology<br />
<strong>of</strong> HSZ and in the fourth group two papers<br />
on the interaction <strong>of</strong> deformation and metamorphism.<br />
In the fifth group there are two<br />
papers on phenomena related to HSZ in rocks<br />
and in the final group there are two papers<br />
on numerical modeling applied to HSZ.<br />
<strong>The</strong> inclusion <strong>of</strong> a comprehensive index at<br />
the rear is a good. I will briefly comment on<br />
some <strong>of</strong> the papers I found most enlightening<br />
given my current research interests.<br />
Sidman et al demonstrate the use <strong>of</strong> the<br />
AMS method as a robust indicator <strong>of</strong> fabric<br />
over a wide range <strong>of</strong> deformation conditions<br />
using the Bitterroot shear zone, Western<br />
Montana. <strong>The</strong>y advocate the rolling-hinge<br />
model for exhumation <strong>of</strong> the Bitterroot core<br />
complex, which is in fact a magma-dominated<br />
core complex. J-P Burg et al document<br />
shear zones in the middle crust-upper mantle<br />
<strong>of</strong> the Kohistan palaeo-island arc. <strong>The</strong>y show<br />
that shear strain localisation began within<br />
compositional gradients and that anastomosing<br />
patterns <strong>of</strong> shear zones develop in<br />
gabbros more commonly than diorites and<br />
granites. <strong>The</strong>ir sketches <strong>of</strong> anastomosing<br />
ductile shear zones resemble those we’ve<br />
observed in the Wyangala Batholith.<br />
Teyessier et al use a range <strong>of</strong> datasets to<br />
suggest the Cordilleran orogen collapsed<br />
through the development <strong>of</strong> channel and<br />
rolling-hinge detachments. <strong>The</strong>y use the Rey<br />
et al (2001) gravitational collapse model<br />
for continental crust to critically test the<br />
tectonic development <strong>of</strong> the Shuswap MCC.<br />
Passchier et al document a different<br />
deformation in a gently dipping, ductile<br />
shear zone over a core complex from China.<br />
<strong>The</strong>y suggest simple shear in the top <strong>of</strong><br />
the shear zone and non-coaxial flow with<br />
volume increase and stretching by vein<br />
intrusion towards the footwall, which they<br />
call an ‘expanding-footwall shear zone.’<br />
High strain deformation tests on natural<br />
gympsum aggregates in torsion by Barberini<br />
et al suggest that gypsum in nature will flow<br />
plastically at shear stress levels lower than<br />
those expected from previous studies. This is<br />
due to dynamic recrystallisation at temperatures<br />
lower than that which causes gypsum<br />
dehydration.<br />
This compilation <strong>of</strong> papers is <strong>of</strong> a universally<br />
good standard and clearly aimed at structural,<br />
tectonic and metamorphic geologists<br />
within academia. <strong>The</strong> price will deter some<br />
from purchasing this volume despite the<br />
currency <strong>of</strong> the papers.<br />
PAUL LENNOX<br />
Regolith Landscape<br />
Evolution across <strong>Australia</strong>:<br />
a compilation <strong>of</strong> regolith<br />
landscape case studies with<br />
regolith landscape evolution<br />
models<br />
Anand R R & de Broekert P (eds)<br />
2005<br />
CRC LEME<br />
354 pages ISBN 1 921039 30 2<br />
$30<br />
www.crcleme.com.au<br />
and<br />
Regolith Expression <strong>of</strong><br />
<strong><strong>Australia</strong>n</strong> Ore Systems:<br />
a compilation <strong>of</strong> exploration<br />
case histories with<br />
conceptual dispersion,<br />
process and exploration<br />
models<br />
Butt C R M, Robertson I D M, Scott K M &<br />
Cornelius M (Eds)<br />
2005<br />
CRC LEME<br />
420 pages ISBN 1 921039 28 0<br />
$30<br />
www.crcleme.com.au<br />
<strong>The</strong> editors <strong>of</strong> these two volumes and their<br />
many contributors have done anyone with<br />
even a passing interest in the <strong><strong>Australia</strong>n</strong><br />
regolith a great favour in bringing together a<br />
large number <strong>of</strong> case studies <strong>of</strong> regolith<br />
development both as a characteristic <strong>of</strong> the<br />
regions and as it relates to the occurrence <strong>of</strong><br />
ore bodies around the continent. <strong>The</strong> volumes<br />
are greatly enriched by introductory review<br />
chapters on the science and applications <strong>of</strong><br />
the regolith.<br />
<strong>The</strong> reviews are <strong>of</strong> <strong><strong>Australia</strong>n</strong> regolith and<br />
landscape patterns (Anand, reproduced in<br />
both volumes); regolith age determination<br />
(Pillans) and regolith-landform mapping<br />
(Craig) in Anand & de Broekert; ore deposit<br />
types (McQueen), sampling media (Butt et al)<br />
and geochemical dispersion (Butt) in Butt et<br />
al; and, very briefly, <strong><strong>Australia</strong>n</strong> climate (Butt)<br />
and vegetation (Butt) patterns (both<br />
volumes). <strong>The</strong> longer chapters are excellent<br />
TAG December 2006 | 37