1. Abstract:
The studying Zone is located in east corner of Yazd and north east of Bafgh and north east,
east to south east of Behabad. It is surround by Behabad fault 1 and Behabad fault 2 as a
horst. The oldest geological outcrops are related to Deviation. Majority most important units
are related to from Iran's geological partitions view point, this area is located in technic –
sedimentary Zone of Iran's central parts and in space between Tabas and PoshtBadom blacks,
and it is mostly located in Tabas black. From structural aspects, have we have lots of
important faults which have employed an absolute role about gathering geological history's
and mineralization of the Zone. Famous faults of the Zone are kohbanan fault, Behabad fault
1 and Behabad fault 2 kohbanan fault is separator of posht Badam block from Tabas block
and Behabad fault 1 is separator of Behabad plain from tectonical Zone of Abdoghi- Ravar.
General trend of faults is North west- southeast and north east- south west.
In the studying area, there are variety of indirections and mines that 8 cases of them consist of
Pudan, Abheidar, Dareshor, Rilkalaghi, Gicher kooh Dehasgar and gojer, have been studied
during last years, majority of mineral materials of these deposits and indication have a vein
shape, and it is so rave to find concordant mineralization or stratifications. Reins usually
fallow structural trend of deposits in lots of cases we can find carbonate units brecciated and
resulted breccia which are replacement of ore and gangue minerals because of tectonically
movements. Mineralization is from the type of Mississippi and stratabound. From
mineralization time controlers aspect, in a conceptual model, tectonically mineralization of
the 2 one is like mineralization hose of late palezoic – Tryasic like past symirian and
hersinian tectono magmatic phase. From mineralization's location controlers aspect, it is
located in tectonic- metalogenic province of Iran's central parts.