It is a very difficult problem to directly determine fluid pressure during hydrocarbon migration and accumulation in sedimentary basins. pVt modeling of coupling hydrocarbon fluid inclusion of its coeval aqueous fluid inclusion provides a powerful tool for establishing the relationship of formation pressure evolution with time. Homogenization temperature of fluid inclusion can routinely be measured under microthermometric microscopy. Crushing technique has been employed to obtain the composition of fluid inclusions, and the commercial software VTFLINC easily and rapidly completes the construction of p t phase diagram. The minimum trapping pressure of hydrocarbon fluid inclusion would be then determined in the p t space. In this paper, three samples of YC21 1 1 and YC21 1 4 wells at YC21 1 structural closure, Qiongdongnan basin, South China Sea, were selected for the pVt modeling practice, and the formation pressure coefficient (equals to fluid pressure/hydrostatic pressure) changing trend with time has primarily been established. The modeling results also indicate that the reservoirs of Lingshui and Yacheng formations in YC21 1 structure are within a very high potential system and would have undergone a discharging of thermal fluids through top seal rupture, which depicts that there is a very high risk for natural gas exploration in this area. It is a very difficult problem to directly determine fluid pressure during hydrocarbon migration and accumulation in sedimentary basins. PVt modeling of coupling hydrocarbon fluid inclusion of its coeval aqueous fluid inclusion of a power tool for establishing the relationship of formation pressure evolution with time. Homogenization temperature of fluid inclusion can routinely be measured under microthermometric microscopy. Crushing technique has been employed to obtain the composition of fluid inclusions, and the commercial software VTFLINC easily and rapidly completes the construction of pt phase diagram. then determined in the pt space. In this paper, three samples of YC21 1 1 and YC21 1 4 wells at YC21 1 structural closure, Qiongdongnan basin, South China Sea, were selected for the pVt modeling practice, and the formation pressure coefficient (equals to fluid pressure / hydrostati c pressure) changing trend with time has been established. The modeling results also indicate that the reservoirs of Lingshui and Yacheng formations in YC21 1 structure are within a very high potential system and would have undergone a discharging of thermal fluids through top seal rupture, which depicts that there is a very high risk for natural gas exploration in this area.