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The Upper Permian Changhsing Formation is one of the most important gas-bearing formations in the Eastern Sichuan Basin. Nonetheless, the primary factors controlling the reef-shoal gas reservoirs of different regions are diverse. Clarifying the controlling factors for the formation of intra-platform reef-shoal reservoirs will promote the exploration and development process of the Changhsing Formation. By using outcrop data, core observation, thin section identification, scanning electron microscope analysis, physical property study, and logging interpretation, this paper analyse the characteristics and factors controlling the reef-shoal reservoir in Dianjiang area of the Eastern Sichuan Basin. The results show that the reef cap and reef base microfacies fine-to-medium crystalline dolomite reservoir have the best physical properties, and the reservoir spaces are primarily composed of intercrystalline pores, intercrystalline solution pores, karst caves, and fractures. The main lithology of reservoir formation is reef-shoal facies. The results for the carbon and oxygen isotopes show that dolomites of different particle sizes are formed in three environments. Affected by regression in the late Changhsingian Age, the reef-shoal of the Changhsing Formation were subaerially exposed to meteoric water diagenesis environments, resulting in the highly dispersed particles in rocks that formed a honeycomb karst system, which greatly improved the physical properties of the reservoirs. After reflux dolomitization, the honeycomb karst system was well preserved due to strong resistance to pressure and dissolution of dolomite. Therefore, dolomitization in the Changhsing formation contributed to reservoir porosity. Later, tectonic fracturing has adjusted and modified the reef-shoal reservoir. In summary, penecontemporaneous karstification was the key to the formation of the reef-shoal reservoir. [ABSTRACT FROM AUTHOR]

The Sinian Dengying Formation in China hosts one of the oldest gas-bearing reservoirs in the world. With a long geological history, it has developed into the reservoir rocks, whose quality depends on chemical dissolution and cementation. Despite presence of cavities and pores in the algal dolomites of the Dengying Formation, they were mostly filled with various forms of dolomite cements. Therefore, the investigation of these dolomites and their evolution is significant for analyzing the mechanism of pore space preservation. There are five types of cements in the Dengying Formation, which were well sampled for lab measurements such as thin section, cathodeluminescence, minor elements, isotope analysis of carbon, oxygen and strontium, in attempt to explore the fillers' geochemical characteristics and the diagenetic fluids. They are characterized as follows: firstly, fibrous rim dolomite cement is a typical product formed at sea bottom, and geochemically very similar to the matrix (micrite and microcrystalline dolomite), which could be a reflection of the geochemical characteristics of water at that time; secondly, the diagenetic fluids of the foliated dolomite cements tend to be inheriting, derived from the shallow burial 'imprisoned' seawater; thirdly, fine- to medium-grained dolomite cements with fairly high strontium isotopes and low carbon and oxygen isotopes were precipitated chiefly in freshwater during the period of uplifting caused by Tongwan tectonic movement; fourthly, coarse-grained dolomite cements bear a relatively high percentage of Mn element, but low in Fe and Sr, with carbon and oxygen isotopes remarkably shifted to negative values, which all show that they are related to hydrocarbon maturation and migration, and corresponding Thermochemical Sulfate Reduction; lastly, saddle-shaped dolomite cements are hydrothermally associated, and they were formed in high-temperature brine, which had passed through the areas rich in radioactive strontium isotopes. [ABSTRACT FROM AUTHOR]