The polycrystalline samples of Zn-doped Fe1−xZnxCr2S4 (0.1⩽x⩽0.9) have been studied with x-ray diffraction, magnetization, and Mössbauer spectra measurements. Magnetic structure transforms from the ferromagnetic (0.1⩽x⩽0.5) to the antiferromagnetic phase (0.7⩽x⩽0.9). The Mössbauer spectra of Fe1−xZnxCr2S4 show asymmetrical eight lines due to electric quadrupole interactions below 10K. The magnetic hyperfine field and electric quadrupole interaction for the sample x=0.5 at 4.2K have been fitted with Mössbauer hyperfine parameters of Hhf=116kOe, θ=27°, φ=0°, η=0.60, EQ=2.28mm∕s, and R=2.9. We have observed that the magnetic hyperfine field Hhf decreases with increasing Zn concentration in the ferrimagnetic range (0.1⩽x⩽0.5) at 4.2K, while it increases in the antiferromagnetic region (0.7⩽x⩽0.9). This indicates the changes in the orbital current field contribution depending on Zn concentration in Fe1−xZnxCr2S4.