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The southeastern margin of the Yangtze Block is a suitable region to decipher Neoproterozoic to Early Paleozoic polyorogenic deformation of the South China Block. Based on 1:50,000-scale geological mapping, four deformational phases were identified through structural analysis and 40Ar/39Ar dating. The earliest event (D1) corresponds to nearly E–W-striking folding and top-to-the south thrusting, developed...
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