er
he
ity
ds
he
he
nd
th
ds
ng
1al
tra
be
ed
on
he
In
tra
ith
all
ils
ca,
yh-
xel
3x3 meters). Forward and reverse intensity, hue,
and saturation (IHS) transforms (Haydn et al.,
1982) were applied to the TM color composite. In
the reverse transform to the RGB (red, green, and
blue) domain, the intensity and the saturation
channels were replaced by the aerial photograph
and by the TM-1 band, respectively. The objective
of such procedure was to generate an image with
high spatial resolution and spectral information
retained from the TM bands. The replacement of
the saturation channel by the TM-1 band was to
enhance the areas of hydrothermal alteration,
because this band presents the best contrast
between altered and unaltered materials (Figure
2). The resulting hybrid product with the spatial
resolution of the aerial photograph and the
spectral information derived from the Landsat
TM bands facilitated the identification of the
areas of hydrothermally altered materials, and the
mapping of the main faults that cut across the
study area.
In order to produce a generalized map showing
the main lithological/physiographical domains
present in the study area, a segmentation
technique that uses a region growing method was
applied to the hybrid images. A segmented image
was obtained which showed a number of
homogeneous regions whose pixels can be
assumed to belong to the same class. The
segmented image was classified using a
supervised region classifier method which
identified four different classes of homogeneous
regions. Field data were used to identify each
classified region. Based on the classified image a
map of the study area was produced (Figure 3)
which showed a very accurate delineation of the
areas of hydrothermally altered materials.
S. CONCLUSIONS
The results showed that a simulated
natural color composite of Landsat-TM images
was a very efficient tool to map hydrothermally
altered materials in vegetated terrains. For the
natural conditions of the study area, target areas
were discriminated even when vegetation covered
up to 60% of the terrain surface.
9
ACKNOWLEDGMENTS
This research was supported by a FAPESP grant
3822-8-88. The authors also thank Oriente Novo
Mining Co. for providing support for field work.
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