Scientific Quarterly Journal of Geosciences

Scientific Quarterly Journal of Geosciences

Sedimentological study of the Sangerd drainage basin in Sabzevar

Document Type : Original Research Paper

Authors
1 Department of Geology, Faculty of Science, Ferdowsi University of Mashhad , Iran
2 Department of Geology, Islamic Azad University, North Tehran Branch, Tehran, Iran
3 Department of Geology, Islamic Azad University, North Tehran Branch, Tehran , Iran
4 Department of Geology, Islamic Azad University, Mashhad Branch, Mashhad , Iran
Abstract
The Sangerd drainage basin is located in central part of Khorasan Province in arid to semiarid climate conditions and consists of three subbasins. Structurally, the study area is a part of Central Iran zone, and is composed of Mesozoic and Cenozoic rocks. The river channels are mainly single with sandy gravelly bedload. The presence of shale and marl as well as seasonal rainfall in the study area, causes the strong erosion. Based on sedimentological studies, 9 lithofacies have been identified. The majority of sediments are sandy gravel (sG) but in downstream they change to gravelly muddy sand (gmS). Geologically, the presence of less resistance sedimentary rocks causes to produce a lot of sediments that can fill Sangerd reservoir very quickly. There for, we suggest by changing the hydraulic condition of channels can decrease the erosion and sediment transport.
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Volume 12, 45-46
Autumn & Winter 2003, Vol. 12, No. 45-46
Winter 2002
Pages 36-47