WANG Yong; ZHONG Jianhua; CHEN Hao; LI Guoying and JIANG Lin
, 2006, 33(5): 1383-0.
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Through the analyses of various data, including thin section analysis, SEM, carbonate content, reflectance of vitrinite, clay, reservoir property and others, it is found that the corrosion of the acidic compositions of feldspar, carbonate, sulfate, etc., is the key factor for the generation of reservoir secondary pores. With burial depth, the corrosion degree of carbonate decreases and that of feldspar increases. The main types of the secondary pores are intergranular pores, intragranular dissolved pores, cement dissolved pores, moldic pores, and fractures. Vertically, there are four secondary pore systems distributed in the formations from 2375m to 2675m, from 2975m to 3350m, from 3675m to 4200m, and below 4500m. The mechanisms of genesis include: thermal evolution of organic matter, experiments indicate that the thermal degradation makes kerogen produce a large amount of organic acid before it goes into the oil-generation windows; abnormally high fluid pressure, the fluid thermal cycle convection and curtain-draining hydrocarbon will enlarge oil-generation windows and lead to the forming of secondary pores; eluviations at unconformities or fracture zones produce weathered crust secondary pores.