Writers : Asgarpour, Zahra; Khatib, Mohammad Mahdi
Refference : 27th Symposium on geosciences and the 13th symposium on geological society of Iran-Tehran
Publishing Year : 1388

Abstract :

North Birjand anticline is a flanking fold, that has been localized in the neogen and quaternary deposits. Various morphotectonic evidences in this anticline establish its activity. The most important of these phenomena is diference in drainage feature in the northern and southern flanks and also from east to west. The fractal dimension of the dranage compression in the northern, southern, eastern and western flanks are 0.825, 0.708, 0.748 and 0.701, respectively. So that fractal dimension in the southern flank is less than northern flank. That showing up the more uplifting and slopping of this flank. Because of the main thrust on the area is Northward dipping and as of the Northern block Is hingging wall block.

Subject List : Fractal analysis