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The structures and trends were assessed with relation to the
deformational events that the region had undergone. Hence a
structural chronology has been outlined.
Careful analysis of the satellite imagery indicated that
the topographic nature of the area is related directly to
the underlying geology; this is an area that is sparsely mapped
and in which the structural configuration is only poorly understood.
A field survey and potential seismic survey was planned directly
from structures identified on the imagery.
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