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10) in the plain; in this part of the basin, B, C and F types (downstream) are present; in some short distances the multi-channel type (D) may occur. The Qara-Chay bed in mountainous part gravelly facies (Gms and Gm) are present; sandy facies (Sm, Sh and St) are more abundant in the plain. Muddy facies (Fl and Fm) persist in distal parts. These facies were mainly deposited in the lower-flow and the primitive stage of the upper-flow regime.]]>
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