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THE Early Ordovician Baiyungang Formation limestone in Tarim is characterized by multiplemagnetic components including primary remanent magnetism (PRM) and late remagnetiza-tion. Considerable attention should be paid to its petromagnetic significance. Investigatingthe relationship between these components and the magnetic carriers is important to distin-
THE Early Ordovician Baiyungang Formation limestone in Tarim is characterized by multiple magnetic components including primary remanent magnetism (PRM) and late remagnetiza- tion. Investigating the relationship between these components and the magnetic carriers is important to distin-