Writers : Moussavi, Seid Morteza; Moshaverinia, Javad
Refference : 9th symposium of geological society of Iran, Tehran, Teacher Training university
Publishing Year : 1384

Abstract :
Pattern of cones of the detritus is the end erosion-sedimentation system which in changing rate and tape 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 : mountain_front