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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

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