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Analysis of Pore Properties of Favorable Shale Oil Reservoir of Chang-7 in Ordos Basin
WANG Xiaowen, GUAN Ping, LIANG Xiaowei, DING Xiaonan, YOU Yuan, ZHANG Chi, FENG Shengbin, ZHANG Jihua
Acta Scientiarum Naturalium Universitatis Pekinensis    2021, 57 (3): 459-469.   DOI: 10.13209/j.0479-8023.2021.018
Abstract735)   HTML    PDF(pc) (32074KB)(108)       Save
Taking well YJ1 as the research object, the pore variety of shale oil reservoir of Chang-7 member in Ordos Basin is characterized qualitatively and quantitatively by using scanning electron microscope and high pressure mercury injection technology. The movable fluid in reservoir is researched by using nuclear magnetic resonance technology, and the main controlling factors affecting the difference of reservoir quality are discussed in detail. The results show that the lithology of high-quality shale oil reservoir in Chang-7 member of Ordos Basin is mainly fine-grained?very fine-grained lithic sandstone, and the sedimentary facies are mainly sandy clastic flow deposition. The reservoir pore types include primary intergranular pores and secondary dissolution pores, and the proportion of intergranular pores is more than that of dissolution pores. According to the type of pore variety, the reservoir can be divided into three types, among which the type I reservoir is the most high-quality reservoir in the study area, with good porosity and permeability. The mobility of reservoir fluid in the study area is mainly affected by the properties of pore variety, the mobile fluid is mainly stored in the macropores, and the effective pore volume is the factor restricting the mobility of fluid. The sand body caused by sandy clastic flow in the study area is a necessary condition for the formation of high-quality reservoir. The proportion of skeleton particles and cement in the rock is the key for the change of reservoir properties. When the skeleton particles increase and the cement content decreases, it is easy to form high-quality reservoir.
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Study on the Development Law of Structural Fractures of Yanchang Formation in Longdong Area, Ordos Basin
ZHAO Wentao, HOU Guiting, ZHANG Juzeng, FENG Shengbin, JU Wei, YOU Yuan, YU Xuan, ZHAN Yan
Acta Scientiarum Naturalium Universitatis Pekinensis    2015, 51 (6): 1047-1058.   DOI: 10.13209/j.0479-8023.2015.064
Abstract1170)      PDF(pc) (1328KB)(1114)       Save

In order to study the distribution of fracture controlled by layer thickness and lithology, clastic rock of 6-7th Member, Yanchang Formation in Longdong area is selected as investigated subject, and the areal density of their structural fractures is meassured. Measured fracture densities show that the layer thickness of clastic sequence has an effect on fracture density. Compared with thicker layer, it is easier for thinner layer to develop structural fracture, which is related to the different stress concentration near fracture tip in different layer thickness. Within a certain thickness range, fracture density has an exponential relationship with layer thickness, while the fracture density remains mostly unchanged when thickness exceeds 250 cm. Under the condition of same layer thickness and different lithology, the value of fracture densities from small to large follow the order of medium sandstone, fine sandstone, siltstone and mudstone, which means that in the same tectonic setting and layer thickness, the smaller the size range is, the larger the fracture density will be. Besides, there is an exponential relationship
between fracture density and grain size, which may be caused by the different stress between grains of different size. By multivariate statistics and mechanism analysis, layer thickness is the key factor in controlling fractures’ development compared with lithology.

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