LAUSR

Abstract Overpressure is an essential factor that controls the accumulation and distribution of oil and gas. In this study, we systematically studied the effects of overpressured fluid activities on the diagenesis and diagenetic evolution of reservoirs in the DF11 Block of the Yinggehai Basin, the South China Sea. The employed methods included thin-section observation, scanning electron microscopy, geochemical analysis of formation water, and C-O isotopic study. The formation water in the DF11 Block was classified as NaHCO3-type continental sedimentary water, showing high HCO3− content and extremely low concentrations of Ca2+ and Mg2+. The formation overpressure drove the carbonate ion-bearing thermal fluid flowing into the top boundary of the overpressure. The carbonates ions were re-precipitated from the fluid due to decreasing pressure and temperature. As a result, a tightly plugged zone that consisted of high carbonate cement content was formed. On the other hand, the overpressure reduced the sources of carbonate cement and limited the secondary growth of quartz by inhibiting the transformation of clay minerals. Consequently, the primary pores in the reservoir were largely preserved. Furthermore, the overpressure increased the solubility of CO2 and generated a large amount of H+ ions in the CO2-rich reservoir, which promoted the dissolution of feldspar and cements in the reservoir. The formation overpressure restrained the mechanical compaction, enhanced the dissolution of minerals, and restricted the cement production, all of which facilitated the formation of high-porosity and mid-depth overpressure reservoirs in the DF11 Block.