The distribution, fractal characteristic and thickness estimation of silty laminae and beds in the Zhangjiatan Shale, Ordos Basin

被引:0
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作者
Key Laboratory of Petroleum Resources Research, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China [1 ]
不详 [2 ]
不详 [3 ]
不详 [4 ]
机构
来源
Nat. Gas Geosci. | / 5卷 / 845-854期
关键词
Digital storage - Flow of fluids - Thickness measurement - Metamorphic rocks - Shale gas;
D O I
10.11764/j.issn.1672-1926.2015.05.0845
中图分类号
学科分类号
摘要
The Zhangjiatan shale of the Lower Chang 7 member of Yanchang Formation, Ordos Basin is an important exploration target for shale gas. Since the silty beds/laminae in the shale play an important role in gas storage, fluid flow, fracturing and development of shale gas/oil, it is of great significance to ascertain the thickness and the distribution characteristic of the silty beds/laminae. The measurement results from outcrop, core and thin section show that the silty beds/laminae have larger detrital grains than those in the clayey laminae and the silty laminae thickness mainly ranges from 0.5mm to 8mm. Their total thickness can occupy 7%-26% of the shale formation with an average density of 8-40 layers/m, which shows strong vertical heterogeneity. The thickness distribution of silty beds/laminae presents a fractal distribution on a dm to mm scale and the fractal dimension D has scale invariance over the whole thickness range. According to the data from the relatively thick layers of silty beds, the accumulative number of the thinner silty beds/laminae was estimated using the Number-size model. The accumulative thickness of silty beds/laminae and its ratio to the shale formation thickness were calculated. It has been verified that this method can ascertain the thickness of the silty beds/laminae effectively. ©, 2015, Science Press. All right reserved.
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页码:845 / 854
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