Microscope, LA-ICP-MS, (Micro)FT-IR, UV-Vis, Raman and other methods were used to analyze conventional gemology, chemical element content and spectral features of Pakistan peridot, so as to discuss its origin characteristics. The result shows that Pakistan peridots contain black Vonsenite-Ludwigite needle and punctiform msgnetite. Compared with peridots from the USA, China, Ethiopia, Vietnam and Madagascar, Pakistan perdots have higher Li, B, Sc but lower Zn, Cu, with relatively lower V/Sc ratio. The absorption bond around 3 580 cm^-1 in the infrared absorption spectrum of peridot in Pakistan is related to the [Si]=(4H)_Si^X substitution mechanism, indicating that the crystal structure contains a certain amount of structural water. The strong absorption near 380, 450, 490, 635 nm in UV-Vis spectrum is related to O^2-→Fe³⁺ transition, ⁶A₁→⁴A₁+⁴E(⁴G)in d-d transition of Fe³⁺ and ⁵T_2g→³T₂, ⁵T_2g→³T_1g electron transition of Fe²⁺. It is concluded that inclusion, trace element and structural water-induced infrared absorption band can be used as the origin identification characteristics of peridots in Pakistan.