The Structure of
Potash and Salt on Diapir Pol,
Zagros Fold-Thrust
Farhadi, Reza1, Christopher J. Talbot2
(1) Geological Survey of
The Zagros fold-thrust belt extends
from East Anatolian left-lateral strike-slip fault in the northwest to
Finally, the flow of salt was ceased moderately then salt was
eroded by rivers flowing mainly eastward; maximum amount of potassium in the
brines is 70 gr/lit and numerous potash boudins (more competently than salt) on Diapir
Pol are the source. The outcrops are two types, iron
rich type and white potash (sylvite is 59.64%, and
the surface reserve is one million tons).
Sketch maps of the three sets of deformation structures by Prof.
C.J. Talbot at the scale of 1/10000 indicated thet
the structural levels or horizons of potash boudins
are quite close to each other and he showed their stratigraphic
extrapolations. Large scale mapping suggest strongly thet
all potash boudins dispersed along the same stratigraphic level which Talbot introduced and he called
it the Zone of Potash Bearing Strata (ZPBS).
The Zagros fold thrust belt with its numerous hydrocarbon
fields is the most resourceprolific fold-thrust
belt of the world but we must review the topics: 1- The stratigraphy
of Hurmoz sequence. 2- The economic aspects of the Prototethys basin.