Magnetic fabric is a manifestion of anisotropy of magnetic susceptibility in rocks. Magnetic fabrics with different geneses have different features. In recent years, geologists have taken some effective researches on the emplacement and deformation features of granitic plutons using magnetic fabric analysis. The Linglong granitic pluton is in the north of the Linglong Composite Batholith in the Northwest of Jiaodong Pennisula, Shandong Province. The pluton has a close spacial relationship with gold deposits. The famous Jiaojia gold mine field and Linglong gold mine field are all in the margin of the pluton. The magnetic fabric features of Linglong granitic pluton and their relationship with gold deposits were studied. The mean degree of magnetic anisotropy is 1.2872, which means typical deformational genesis. The strike of magnetic foliations is circling Beijie granodiorite pluton with gentle dips; the magnetic lineations are almost horiziontal with NW trending. The research revealed that the deformational magnetic fabric is formed during the instrusion of Beijie granodiorite pluton; besides the control of faults to the gold deposits, the degree of magnetic susceptibility anisotropy and gold deposits have aslo a close spacial relationship. The gold deposits are located in places where the degree of magnetic susceptibility anisotropy is larger; otherwise, the gold deposits are very poor.