— 
Faults of the IS'order = Supposed faults 
_— 
Faults of the II^d order Y Thermal - mineral springs 
Fig. 2. The map of the faults based on 
the Landsat imagery with thermo-mineral 
springs in area of the NW part of Yugo- 
slavia 
EXPLORATION. OF ORE OCCURENCES 
On the Landsat images have been registered by morpho- 
structural analysis of the relief beside ruptural deformations al- 
so geomorphological ring forms were discovered. 
It is known that the polymetal ores are mostly relationed 
to magmatic and tectonic activity. About 50% of ore are on the big 
faults crosses layers (Colective authors, 1976, page 95). It has 
been found out that the majority of ore layers in the area of Ne- 
vada is located along the bigger faults, which may be identified 
on the Landsat images (Sabins, 1978, page 279). 
Resulting that the large faults of the major channels 
through which circulates hydrothermal solution, so that there is 
the depositing and cristallization of minerals. 
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