摘要
Carbonate sequences of the upper Ordovician Lianglitag Formation along the Tazhong 83-Tazhong 16 well blocks, Slope Break I, Tarim Block is 170~300 m thick and notable as reservoirs of oil-gas. Based on the analysis of drilling cores, thin sections and logging parameters, types of reservoir space are recognized as cave, intragranularly dissolved pores, intercrystalline dissolved pores, moldic pore, biologic dorsal pore, organic framework pore and micro-fracture. The features of the void structures as well as their associations are catalogued as vug, fracture-vug,and fracture configuration types, respectively, and are in similar abundance. Therefore, the authors consider it a potential area for high quality type I andⅡ reservoirs.