Geochemical Analysis of Dolomite in the Fourth Member of the Upper Sinian Dengying Formation, Northern Sichuan Basin, China

The fourth member of the Sinian Dengying Formation in northern Sichuan was reformed by multistage diagenetic fluids. It is beneficial to systematically analyze the diagenetic evolution of the area to clarify the sedimentary evolution of the dolomite in the fourth member of the Dengying Formation and the fluid characteristics at different diagenetic stages. In this study, the petrological characteristics, vertical sedimentary evolution, diagenetic fluid stages, and diagenetic environment of Dengsi dolomite were analyzed by using carbon-oxygen strontium isotopes, rare-earth elements, major and trace elements, combined with the supporting thin section identification and cathodoluminescence techniques, and the source and properties of diagenetic fluid of Dengsi dolomite in different diagenetic environments were determined. The results show that (1) during the deposition period of the fourth member of the Dengying Formation, the water body showed a trend from shallow to deep and then steadily to shallow, which was in a shallow freshwater reducing environment and had a warm and humid paleoclimate environment; (2) the dolomite of the fourth member of Dengying Formation in northern Sichuan is less affected by terrigenous materials. The C and O isotopes of dolomite are generally negative at the top of the fourth member of the Dengying Formation, and the top of the formation is obviously transformed into rock by atmospheric fresh water; rare-earth elements show that dolomitized fluid is dominated by primitive seawater, and the marine fluid from or flowing through the carbonaceous shale formation rich in feldspar minerals in the Qiongzhusi formation during burial period makes the rare earth elements show obvious positive EU anomalies. The high Sr-87/Sr-86 ratio of the surrounding rock and cement is caused by the Sr-87-rich marine fluid coming from the fault communication or along the unconformity zone; (3) since the deposition of the dolomite of the fourth member of Dengshan formation in northern Sichuan, it has experienced multistage diagenesis. The multistage cement and fillings in the pores have recorded at least seven stages of fluid activity history: during the quasi-contemporaneous period, fresh water was transformed to increase pores, and seawater was cemented to damage pores. During the supergene period, the pore size of atmospheric freshwater increased generally; during the middle deep burial period, the acid fluid was reformed to increase the porosity, the Sr-87-rich hydrocarbon-bearing fluid was used to fill the damaged pores, and the Eu2+-rich marine source fluid was used to fill the damaged pores. In the deep burial period, siliceous hydrothermal fluid filled the damaged hole.