鄂爾多斯盆地甘泉地區(qū)延長組長7段頁巖氣儲層特征研究
[Abstract]:The successful exploration and development of marine shale gas in North America have provided important inspiration for the study of shale gas in China. However, the geological conditions of China's lacustrine shale gas reservoirs are different and the contents of brittle minerals are relatively low. The related theories can not be applied directly, so it is a new focus of unconventional oil and gas geology to study shale gas reservoir characteristics according to the actual conditions in different regions of China. Two sets of semi-deep lacustrine-deep lacustrine shale have been developed in the Triassic Yanchang formation of Ordos Basin. Recent successful drilling of several shale gas wells in the southeast of the Yishan slope has proved that this area has suitable conditions for shale gas formation and great exploration potential. Accurate determination of shale gas reservoir characteristics is a key issue in shale gas selection evaluation in this area. In this paper, the shale of member 7 of Yanchang formation in Ganquan area, Ordos Basin, is taken as the research object. By using various geological evaluation and experimental analysis techniques, the spatial distribution characteristics, mineral composition and geochemical characteristics of shale gas reservoir are studied. Pore types and physical properties of reservoirs are studied. The main experimental methods and analytical techniques used include XRD mineral composition analysis and measurement, rock pyrolysis, scanning electron microscope observation after argon ion profile, high pressure mercury injection experiment, gas adsorption experiment and pulse attenuation gas porosity test. The main results are as follows: (1) the shale of Chang 7 in Ganquan area is mainly composed of black shale with thin layer of gray and black silty mudstone, gray black fossil mudstone and shaly siltstone. The mineral composition of shale gas reservoir in this area is mainly quartz. Feldspar and clay, in addition to a small amount of carbonate, siderite and pyrite; (3) the pore types of shale gas reservoir can be divided into intergranular pore, intragranular pore and organic pore. Intergranular pore includes clastic intergranular pore and clay mineral intergranular pore. The development degree of organic matter pores is closely related to the maturity of organic matter. (4) the volume of micropores below 2rnm with the pore size of 2-100rnm and the macropores above 100nnm are relatively small in shale gas reservoirs in the study area. The porosity of shale with silty grain layer is higher than that of pure shale in reservoir.
【學(xué)位授予單位】:西北大學(xué)
【學(xué)位級別】:碩士
【學(xué)位授予年份】:2015
【分類號】:P618.13
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