Paleomagnetic data, during the Phanerozoic obtained in the last 20 years in
the Yangtze Block (YZB), are critically reviewed. A new apparent polar wan
der path (APWP) for the YZB is constructed by selected poles with objective
reliable criteria, with a Real of placing constraints on the models of the
formation and subsequent deformation and reconstructing the tectonic evolu
tion history of this region.