Mar 14, 2011018332This paper focuses on Holocene deposits of the Firenze alluvial plain Northern Apennines, Italy and deals with the sedimentary features of chute channels draining the down‐river edges of the meander neck formed by 70 to 100 m wide and 1 to 11835 m deep sinuous channels. Two main types of chute channels have been recognized.Get Latest Price
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