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The East China Sea Shelf Basin (ECSSB) lies among the Eurasian Plate, the Pacific Plate, and the Indian Plate. Its formation and evolution since the Mesozoic was controlled by the combined effect of westward subduction of the Pacific Plate and actions of the large‐scale ductile shear zone on the South China Plate—the Changle–Nan'ao Fault Zone. This paper selects the southern ECSSB with well‐developed...
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