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Whether strain is physically meaningful surely depends on what it's used
for. As a descriptor of change in shape it is very useful, and as
Koenemann says, easy to measure and geometrically well-defined. It is
not useful as a cause-effect relation, but that's not what it's used
for.
 
This debate seems to have lost track of the basics of structural
geology, in particular observations made of deformed rocks in the field.
We already know (I think) that strain is a descriptive term, it does not
describe the underlying deformation mechanisms involved in the change of
shape it describes. Strain is also not a concept used to directly
calculate stress or work done, this requires interpretations of
rheology, as well as the deformation path which, as Koenemann rightly
states, cannot be directly derived from a finite strain measurement.
 
I've found when teaching undergrad courses that strain is a very useful
concept to describe changes in geometry, and it is also very useful to
describe field observations of deformed rocks. I'm still to see any
reference in Koenemann's discourses to observations relating to his
theory. Unless the new theories can be used to improve our understanding
and interpretations of field observations, I struggle to see how it can
be more useful than strain, which is a very useful, and meaningful,
quantity describing the observed geometry of deformed rocks.
 
Ake


 
 
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Dr Ake Fagereng
Department of Geological Sciences
University of Cape Town
Private Bag X3
Rondebosch 7701
South Africa
 
Phone: +27-21-650-2926
e-mail: [log in to unmask]
web: http://web.uct.ac.za/depts/geolsci/people/staff/ake.htm
>>> John Whalley <[log in to unmask]> 2011/04/07 12:57 PM >>>
 
 
 
John S Whalley, Geoscience Programme Manager
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