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Nilanjan Bhowmick AIR 3, CSIR NET (Earth Science)
Rahul kumar
Crevasse splay is a fluvial deposit generally found in river flood plains. It forms when high speed channel currents breach the levee. The deposit associated with crevasse splay is fining upward. Commonly, fine grain sediments are found in flood plains but presence of crevasse splay will result into coarse grained sand deposition into the river flood plain; which can work as a potential reservoir for hydrocarbons.