S U M M A R YWe present a new approach to extract deep crustal velocity structure from short-offset seismic refraction sections acquired over sedimentary basins. A coincident deep seismic nearvertical (NV) reflection stack section is used to constrain the derived crustal structure. The high-amplitude free-surface multiples, often found on refraction sections due to high velocity gradients in shallow sedimentary layers, are routinely modelled for velocity and Q structure of the sedimentary strata. These multiples almost completely mask most of the arrivals, including reflected phases from crustal interfaces. By application of velocity filtering with a rejection band that includes the apparent velocity of the free-surface multiples, they can, however, be significantly attenuated. The relatively weak signals, notably the deep crustal reflections in the subcritical (SC) range, can thus be well developed. This approach is demonstrated here by application to a short-offset refraction section in two steps: initially, the free-surface multiples are modelled for obtaining the sedimentary basin velocity structure, later they are substantially attenuated by velocity filtering to enhance the weak SC reflections, further modelled for the velocity structure of the deep crust underlying the west Bengal sedimentary basin, India. The stack section obtained by processing the deep seismic NV reflection data set, coincident with the short-offset refraction section, is consistent with and well substantiates the derived model of the crustal velocity structure in the region.Near-vertical (NV) common-depth-point reflection profiling and wide-angle (WA) reflection-refraction profiling are the two most successful techniques of the controlled source seismology for exploring the crustal and subcrustal lithosphere. These two techniques, employing different frequencies, reveal different aspects of the structure of the Earth's interior (Fuchs 1986). NV reflection sections delineate structural images revealing the deep tectonic processes and evolution, while WA refraction data provide models of the velocity, Q structure and possible composition of the interior. There exists a substantial range of the subcritical region (SC) between the NV and WA ranges (Fig. 1). The information in the subcritical (SC) region is, however, not routinely used because of the inherently low amplitudes of the signals in that range. In sedimentary basins, which are mostly the exploration targets for hydrocarbons, the structure and composition of the sediments and their basement are of primary interest. The seismic data acquisition in those regions is, therefore, often limited to 5-6 s of recording times by the NV, and out to only 50-60 km recording distances by the WA profiles. Necessary data sets for deep crustal structure in those regions have to be obtained by specially designed experiments of the NV and WA profiling with extended acquisition parameters. While NV reflection imaging to deep crustal depths can be accomplished by extended recording times and multichan...