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Deep-buried marine carbonate reservoirs in the Tarim Basin present challenges for exploration. A regional unconformity in dolomite at the top surface of the Shuiquan Formation makes the carbonate rocks ideal reservoirs. This study determines the unconformity belt distribution, lithology, reservoir space types and the controlling factors of the Shuiquan Formation, to establish a paleokarst development model and predict the favourable exploration targets. By flattening the seismic-event section and tracking truncation points on the seismic profiles, the unconformity area and denudation trends of the Shuiquan Formation are identified. The denudation area appears on a NEE-trending plane as a band with a width of 10–20 km and a thickness that expands from the depression to the slope and uplift. The Sinian Shuiquan Formation developed in a carbonate platform–tidal flat environment. Outcrop, core, well logging, and thin-section observations reveal that the lithology of the Shuiquan Formation consists of crystalline dolomite and granular dolomite, with pore types that include intercrystalline dissolution pores, intercrystalline pores and structural fractures. Unconformity, karstification and tectonic activity with atmospheric freshwater leaching, storage space and communication channels, respectively, are considered crucial factors influencing carbonate reservoir formation in the study area. A prediction model for the carbonate reservoirs in the Tadong area shows that the strong karst belt on the slope is the ideal area for forming a carbonate reservoir.
Cheng et al. (2024) studied this question.