Abstract
In this paper sedimentation process and lateral growth objects in deepwater uncompensated and shallow water epicontinental-paleo basins developed at various evolution stages of South Caspian and Middle Caspian basins are being considered. The role of boundary structures of Scythian-Turan platform in the Middle Caspian and avalanche sedimentation on the continental shelf in development of sedimentation units and specific shape objects of lateral growth in many kilometers long sedimentary cover of South-Caspian basin has been shown. According to the interpretation of seismo-stratigraphic data the inflow of paleodeltaic, avandeltaic and turbidite objects of lateral development for infill of the Early Pliocene basin has been proved
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