Citation: | WANG Yi-xuan, ZHANG Xiao-dong, SUN Yong, AN Xing-yu. THE POROSITY CHARACTERISTICS OF SEDIMENTARY AND DIAGENETIC ENVIRONMENT FOR SHAN-2 MEMBER TO HE-8 MEMBER AT THE UPPER PALEOZOIC IN NORTHERN SHAANXI SLOPE[J]. Journal of Geomechanics, 2014, 20(3): 230-242. |
The typical low permeability lithological reservoir is the main reservoir which has been developed from Shan-2 member to He-8 member at the upper Paleozoic in Northern Shaanxi slope, Ordos Basin. The reservoir properties dominate the enrichment of oils and gas. The merits of tight reservoir porosity are associated with their sedimentary and diagenetic environment. In this paper, the influence of the late-diagenetic on reservoir porosity was discussed according to the sedimentary particle size analysis and scanning electron microscopy observation. From the result of this study, we can draw the conclusion that the chief destructions of reservoir-quality which is in the transform sequence of "Montmorillonite-Andreattite-Illite" are the cementation and the evolution of clay cementation. Furthermore, the clay membrane of chlorite which is developed in the surface of clastic particles can protect the reservoir porosity from the late-cementation while block the primary porosity. Therefore the clay membrane of chlorite can be one of the criteria to judge the reservoir-quality in gas reservoir exploration.
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Tectonic map of Ordos Basin and the studied area
The reservoir lithology classification of study area from Shan 2 to He 8
Scanning electron microscopy for clay mineral and carbonate cementation
The tendency of clay mineral with the buried depth
The vertical characteristics of reservoir from Shan 2 to He 8 members
The relationships between porosity and the grain size of reservoir
The relationships between reservoir porosity and clay mineral content
Relationship between reservoir porosity and the chlorite film
Relationships between porosity and the content of cementation