Writers : Safar Nejad, M.; Moosavi Harami, S. R.; Mahboobim, A.; Khane Bad, M.
Refference : 28th Symposium on Geosciences and the 14th Symposium on Geological Society of Iran
Publishing Year : 1389

Abstract :

The Norozi drainage basin is located southwest of Ghochan with platy shape and surface area about 61 Km2. The Norozi River is mainly gravelly bed load. Grain size change toward downstream is not exponentional, that has two discontinuities and three isolated sedimentary links. These discontinuities are resulted from laterally input of sediments from tributaries, change of lithology, change of bed slope and emergence bed rock. The isolated sedimentary links have fining trend to downstream due to hydraulic sorting and abrasion.

Subject List : sedimentary link