1
زمینشناسی و معدن::
منطقه ذخیره
The tectonic structure of the deposit area has been precised based on the results of geological mapping and technical work.
The depth delineation of deposit has been determined by the erosion level of the deposit area which is 500 m a. s.
During the first one the deposit area was divided into the above described tectonic blocks.
The following tables summarise all the reserves calculated in frame of the deposit area {Table 2) as well as the level reserves delineated within the tectonic block II {Tables 3-6).
On the east side of the saddle the main water way of the region is located - the Galand River, which drains 90 % of deposit area.
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