Converted wave terminologyConversion occurs each time a wave impinges at non-normal incidence on an impedance contrast, and is accompanied by a partition of energy between different wave types (P, S, reflected, transmitted). Some of the possible conversions have such a low energy content that they can be considered negligible for seismic imaging purposes. Moreover, marine acquisition with a towed streamer requires that a P wave must arrive at the receiver. Among the many different types of waves analysed, some conversions appear to be particularly attractive:• PSSP: means P wave down to top basalt, conversion to S wave at top basalt, S propagation and reflection in subbasalt layers up to top basalt, conversion to P wave at top basalt and propagation up to receivers. This is the symmetrical converted wave (for a 1D layered medium, the downgoing and upgoing travel paths have the same wave mode travelling in the same layer) with the minimum number of conversions. Symmetrical waves are very interesting, because they allow the use of traditional processing tools developed for PP waves. • PSP: means P wave down to an impedance contrast, S wave reflected at the contrast up to sea bottom, conversion to P wave at sea bottom and propagation to