Writers : Taghdisi Nikbakht, S.; Mahmoudi Gharaei, M. H.; Mahboubi, A.; Khanebad, M.; Paseban, E.
Refference : 29th symposium on geosciences
Publishing Year : 1389

Abstract :

Eshghabad-Sule watershed with the surface of 81.365 km2 in SW of Quchan, consist of gravelly, sandy and muddy deposits, which are formed Matrix supported Gravel (Gmm), Grain supported gravel (Gem), Grain supported gravel with horizontal bedding (Gh), Sand with horizontal bedding (Sh), Laminated Mud (Fl) and Massive mud (Fm). Existing fades have formed in 6 architectural elements such as Channel (CH), Sandy bed forms (SB), Gravity flow deposits (SG), Gravel bars and Bed forms (GB), Laminated sand sheet (LS) and Fine grain dasstic deposits (FF). Based on identified facies associations and architectural elements, the sedimentary model of Eshghabad - Sule is gravelly braided river system.

Subject List : watershed