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Diagenetic Characteristics and Origin of Abnormal High-Porosity Belt in E2s2 Reservoir of Structure Jinzhou 20-A
详细信息   
摘要


     Comprehensively utilizing the data of cast thin section, scanning electron micrograph SEM , X-ray diffraction, cathodoluminescence/cathodeluminescence and physical properties, the petrological characteristics, di- agenesis, overpressure and secondary pore geneses and so on are figured out for Member 2 reservoir of Shahejie For- mation E2s2 in Structure Jinzhou 20-A. The results show that the sandstone types are mainly feldspathic sand- stone and lithic-feldspar sandstone, which have abundant content of preferring solution; the diageneses main refer to compaction, cementation, metasomatism and dissolution, which are typically characterized by early-stage carbon- ate cementation and later dissolution, the diagenetic evolution is within middle-A stage, which is lagging behind comparing the regional diagenetic evolution; the pressure sure and moreover the pressure coefficient decreases with line of E2s2 formation is parallel to the hydrostatic pres- the depth increases, as a overpressure connecting trans- mission. The dissolution redistribution of the carbonate cements in the overpressure mothballing box and the re- tardation of the clay minerals by the overpressure are the main controlling factors of the generation of the high-poros-ity belts in the deep part.

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