The characteristics of Ordovician paleokarst reservoirs in the Tahe Oilfield are complex. Many prediction studies on the distribution of karst fractures and caves have been carried out, but the filling types and distribution characteristics of caves have been less studied and are thus less understood. First, the development characteristics of the early paleohydrological landforms in the early Hercynian are considered, the paleokarst landforms are restored, the characteristics of the paleohydrological network are clarified, and the lateral distribution of the surface and groundwater systems is illustrated. Additionally, based on a qualitative analysis of core thin section photographs, conventional logging curves, full-bore formation microresistivity scanning, imaging, logging and other characteristics, the existing filling types are divided into four classes: vertical flow filling, river transport filling, cave collapse and hydrothermal transformation. Moreover, reservoir facies division standards for the different filling types are established. Different filling types are constrained in the context of paleogeomorphology and paleohydrology to further study the filling effects and the corresponding controlling factors. As research progresses, five common joint control modes are proposed: joint control of sinkholes and underground rivers, joint control of ancient landforms and underground rivers, joint control of multilayer caves and ancient landforms, control due to collapse and fracture, and joint control of early collapse and late hydrothermal transformation. Based on the model, the relevant mechanisms and the concentrated areas of development are analyzed in depth. The distribution map of the plane filling type is obtained by combining the development model with the identification of the filling type. The relationships between oil and gas production and the reservoir filling degree and between oil and gas migration channels are analyzed by the classification and statistics of different filling types laterally, and the relationships between oil and gas production and the reservoir filling degree and between oil and gas migration channels are analyzed. Hydrothermal action has the strongest ability to transform reservoirs, mainly due to hydrothermal dissolution and fault zones transporting oil and gas; the yield of caves filled with sinkholes is relatively low, which is related to the good reservoir space retained by oil and gas filling and the migration channels provided by fault zones. The yield of the underground river filling type is lower than that of the water-falling cave filling type, mainly because the underground river filling type is located in the karst slope and lower part of the basin. The water energy in the karst slope is relatively strong, and the interior of the cave is filled with medium-fine sandstone. In the lower part of the karst zone, the water energy becomes weak; both of these conditions lead to further filling of the cave reservoir space and a lack of migration channels. The collapse filling type has the strongest impact on the reservoir because this discussion is mainly about late collapse, which causes the cave to collapse, and the internal filling is severe; even if a fault zone acts as a migration channel, oil and gas production is relatively low.
Read full abstract