Upland interfluve (Doab) deposition: Alternative model to muddy overbank deposits

Major alluvial plains contain large tracts of fine-grained muddy sediments, deposited away from the main river channels, which are mostly classed as o verbank or floodplain deposits. Systematic study of the Ganga plain shows t hat such large tracts of deposition of muddy sediments are located several metres above the major channels, and are not flooded by overtopping of the major river channels. These surfaces are here designated as upland interflu ve areas (Doab) where deposition of fine-grained sediments takes place inde pendent of the processes operating in the main channels. The surfaces show distinct depositional domains with characteristic deposits. These include h igher sloping surfaces (mottled silt), lower flat surfaces (variegated clay ey silt), gulleys (sandy silt), small channels (mottled silty sand), ponds (shelly sandy clayey silt), lakes (shelly clayey silt). These deposits are prone to diagenetic changes, especially the development of calcrete horizon s. Redistribution of these domains through time produces characteristic mud -dominant alluvial stratigraphy as observed in the Late Quaternary deposits of the Ganga plain. This succession shows similarity to mud-dominant depos its of the Siwalik succession. These Doab deposits are distinct from the ov erbank deposits formed close to the river channels affected by channel proc esses. It is argued that many of the thick mud-dominant fluvial deposits of the ancient fluvial record are products of deposition in upland interfluve areas.