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We offer to apply the powerful Dynamic Time Warping (DTW) algorithm to findthe spreading rate variation by comparing profiles of marine magnetic anomalieswith the synthetic field constructed by the magnetic polarity reference scale.For the fixed spreading rate and the given interval of the polarity scale wegenerate the synthetic magnetic fields which we compare with the field obtainedfor temporal variations of seafloor spreading rate.

Testing the Dynamic Time Warping algorithm in the Seafloor Spreading Rate Problem