Refference : The 25th Symposium on Geoscience;Tehran
Publishing Year : 1385

Abstract :

In study active tectonic pattern of cones of the detritus is the end erosion - sedimentation system was very important. which in changing rate and taype of sedimentation by rate of erosion due up lifting.
These elements appear useful information about tectonic regime of the area in last and present time.
With this aim, the related factors to this process is studied and appear that the rate of up lifting is access in the central past of the area(with plunge to east).
At present most of, the disturbance appears is related to basins of Central part in the studied area which this conclusion emphasizing by others factors of morphometery and structural information.

Subject List : active tectonic