Fractal features of development degree of Ordovicia paleokarst in the Ordos basin
-
摘要: 鄂尔多斯盆地奥陶系天然气勘探实践表明,古岩溶发育程度影响着储层优劣,然而对古岩溶发育程度的描述缺少定量化手段。本文利用分形理论对鄂尔多斯盆地奥陶系古岩溶的发育程度进行定量化研究,首先分析了古岩溶的分形特征,进而研究了分形维数的计算方法与实现流程,最后结合钻探资料利用分形维数对工区内古岩溶发育程度进行了定量化描述并分析了其与储层优劣的关系。结果表明,鄂尔多斯盆地奥陶系古岩溶的发育具有分形特征,分形维数反映了古岩溶在一定地质条件下的发育程度,工区内工业气流井的分形维数大于1.65。因此,将分形维数作为衡量古岩溶发育程度的定量指标,无疑会提高古岩溶储层评价的客观性、科学性。Abstract: Oil and gas exploration practice shows that the development degree of paleokarst has influence on reservoir quality. However, there is no means of quantitative description for such a feature. This paper analyzes the development degree of the Ordovician paleokarst in the Ordos basin based on its fractal features. First, the fractal features of paleokarst were studied. Then, fractal algorithm was analyzed and its operation flow was designed. Finally, the paleokarst development degree was quantitatively described by fractal dimension combined with the drilling data, and the relationship between fractal dimension and reservoir was analyzed. Results indicate that the development degree of Ordos paleokarst shows fractal features, which reflect the development degree of paleokarst under certain geological conditions, and the fractal dimension of industrial gas wells is greater than 1.65. Therefore, using fractal dimension to classify the development degrees of paleokarst can improve the objectivity and accuracy of reservoir evaluation in areas with paleokarst.
-
Key words:
- Ordos basin /
- development degree of paleokarst /
- fractal features /
- reservoir evaluation
-
[1] 杨华,黄道军,郑聪斌.鄂尔多斯盆地奥陶系岩溶古地貌气藏特征及勘探进展[J].中国石油勘探,2006,11(3):1-5. [2] Mandelbrot B B. How long is the coast of Britain? Statistical self-similarity and fractional dimension [J]. Science, New Series, 1967, 3775(156): 636-638. [3] Mandelbrot B B,Wallis J R. Some long run properties of geophysical records [M]. New York: Plenum Press, 1995: 55-65. [4] Yu J F, Li Z X, Han M L. Fractal and its application to sedimentology [J]. Journal of Coal Science & Engineering(China), 2002, 47(2): 31-37. [5] 刘永顺,冯肖兵,聂保锋. 北京沿河城地区东岭台组酸性火山碎屑流的碎屑分形特征及其成因[J].岩石学报,2014,30(12):3671-3680. [6] 谢晓永,郭新江,蒋祖军. 储层孔隙结构分形特征与损害研究[J].天然气地球科学,2011,22(6):1128-1132. [7] 成秋明. 多重分形与地质统计学方法用于勘查地球化学异常空间结构和奇异性分析[J].地球科学-中国地质大学学报,2001,26(2):161-166. [8] 胡章喜,沈继方. 岩溶形态系统的分形特征及其机理探讨[J].地球科学-中国地质大学学报,1996,19(1):102-107. [9] Sari B, Kusumayudha.M T, Zen S N. Fractal Analysis of the Oyo River, Cave Systems, and Topography of the Gunungsewu karst area, central Java, Indonesia [J]. Hydrogeology Journal, 2000,8: 271-278. [10] 饶华,李建民,孙夕平. 利用分形理论预测潜山储层裂缝的分布[J].石油地球物理勘探,2009,44(1):98-103. [11] Viacheslav A, Tomasz B, Krzysztof D. Fractal dimensions of cave for exemplary gypsum cave-mazes of Western Ukraine [J]. Landform Analysis, 2013, 22(2): 31-37. [12] 刘欢,张长青,贾福东. 西南三江普朗铜矿岩浆混合作用:矿物学和地球化学证据[J].岩石学报,2015,31(11):3189-3202. [13] 李振宏,胡健民. 鄂尔多斯盆地构造演化与古岩溶储层分布[J].石油与天然气地质,2010,31(5):640-647. [14] 杨华,王宝清,孙六一,等. 鄂尔多斯盆地古隆起周边地区奥陶系马家沟组储层影响因素[J].岩性油气藏,2013,25(3):10-16. [15] 侯方浩,方少仙,董兆雄,等.鄂尔多斯盆地中奥陶统马家沟组沉积环境与岩相发育特征[J].沉积学报,2003,21(1):106-112. [16] 陈颙,陈凌.分形几何学[M].北京:地震出版社,2005:30-38. [17] 谢季坚,邓小炎.现代数学方法选讲[M]. 北京:高等教育出版社,2001: 38-42. [18] 张济忠.分形[M].北京:清华大学出版社,2010: 83-89. [19] Mandelbrot B B.The fractal geometry of nature [M]. New York: W H Freeman, 1985: 71-78. [20] 梁虹,卢娟. 喀斯特流域水系分形、熵及其地貌意义[J].地理科学,1997,17(4):310-315.
点击查看大图
计量
- 文章访问数: 1571
- HTML浏览量: 260
- PDF下载量: 752
- 被引次数: 0