In this work we develop a simple methodology to the representation of irregularly distributed data (originally described by two dimensions) in order to map them in an unique dimension along an arc of curve (in particular as triangular functions periodically spaced). It means: it is identified, approximately, the points of a planar region to those belonging to a curve superimposed on the abovementioned region. We apply, with reasonable success, such method to the case of the two-dimensional compressional wave velocity field proceeding from the geologic model of the continental shelf break strongly marked by rugosities. Results show that not big scale variations can influence, in a sensible way, the quality of model representation.
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