The article presents the results of studying the postsedimentary mineralization of productive terrigenous deposits of the Pashiysky horizon of the South Tatar arch. The authors' research was carried out on the basis of a large amount of core material from newly studied wells with the involvement of wells from the archival fund. The analytical work included the following methods: classical optical microscopy and scanning electron microscopy (SEM). Using these methods, the main types of secondary mineral formation, the form and nature of the allocation of authigenic minerals that form secondary cement were studied, and an assessment of the degree of their influence on the filtration-capacitive properties (FPP) was given. It is shown that sideritization is a fairly common phenomenon in the studied deposits, but it does not have a significant effect on the reduction of the reservoir properties of productive deposits. Detailed optical and mineralogical studies have shown that authigenic siderite in the studied rocks is presented in various forms (spherites, spherulites, oolites and granular grains) and is mostly found in silt varieties. In productive sandstones, an insignificant decrease in the reservoir properties can only be associated with expanding rims in siderite spherites. As shown by the study of the composition of these rims, they are composed mainly of ankerite, in places they contain mangano-siderite. In some samples of the Pashiysky horizon, partial replacement of siderite by iron hydroxides was observed; in isolated wells, thin layers of oolitic siderite-ferruginous rocks were encountered. It was shown that the main influence on the reduction of the filtration-capacity properties of the studied sediments is secondary silification and carbonatization. At the same time, secondary quartz is developed mainly in water-saturated sandstones and heterogeneous silt-sandstones, and, as a rule, is distributed mostly locally. Secondary silica is observed in the form of regeneration rims, xenomorphic grains and is deposited on the walls of pores and channels. A significant effect on the reduction of the porosity and permeability parameters of the productive sandstones of the Pashiysky horizon of the South Tatar arch is exerted by secondary crystalline calcite or dolomite island cement of the basal, basal-pore and poikillite type.
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