The East Gobi porphyry molybdenum deposit is a newly discovered super-large ore deposit in Xinjiang. Mineralization occurs mainly in veins dominated by quartz vein and K-feldspar vein so the deposit shares characteristics of quartz vein type deposit and porphyry deposit. Study on fluid inclusions shows that the deposit is a meso-high temperature magmatic hydrothermal fluid Mo deposit formed at shallower depth and at temperature 197 to 390 ℃ and pressure 531.04×105 to 752.10×105 Pa Pa in Hercynian Period.