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时频分析技术在须家河组储层气水判别中的应用
引用本文:肖思和,徐天吉,程冰洁. 时频分析技术在须家河组储层气水判别中的应用[J]. 天然气工业, 2009, 29(11): 41-43. DOI: 10.3787/j.issn.1000-0976.2009.11.012
作者姓名:肖思和  徐天吉  程冰洁
作者单位:1.成都理工大学材料与化学化工学院;2.中国石化西南油气分公司勘探开发研究院德阳分院;3.“油气藏地质及开发工程”国家重点实验室·成都理工大学;4.成都理工大学信息工程学院
摘    要:四川盆地川西坳陷深层上三叠统须家河组的X851井、X856井、X2井、X3井、X10井等一批高产气井证实了该区具有巨大的勘探开发潜力。然而,CX565、X201等高产水井的出现也为该区成功部署井位增添了不确定因素,因此,对该区须家河组储层气水判别就显得尤为重要。地震波在须家河组的含气储层和含水储层中传播时,在时间域内难以发现振幅、频率和能量等动力学属性的变化差异。采用时频分析技术将时间域的地震信号变换到时间-频率域进行对比分析解释,发现“低频阴影”、“高频衰减”等现象在含气储层中十分突出,而在含水储层中却不存在。利用时频域内的这些典型特征建立模式,并对该区含气储层和含水储层进行了有效的区分,其结果与钻、测井资料吻合良好。

关 键 词:四川盆地  西  晚三叠世  致密碎屑岩  流体性质  时间  频率  判别

Application of time-frequency analysis method to the discrimination of gas and water layers in the Upper Tri-assic Xujiahe Formation reservoirs
XIAO Si-he,XU Tian-ji,CHENG Bing-jie. Application of time-frequency analysis method to the discrimination of gas and water layers in the Upper Tri-assic Xujiahe Formation reservoirs[J]. Natural Gas Industry, 2009, 29(11): 41-43. DOI: 10.3787/j.issn.1000-0976.2009.11.012
Authors:XIAO Si-he  XU Tian-ji  CHENG Bing-jie
Affiliation:1.College of Material and Chemistry & Chemical Engineering,Chengdu University of Technology,Chengdu 610059,China; 2.Deyang Branch of Exploration and Development Research Institute, Sinopec Southwest Branch Company, Deyang 618000, China; 3.State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China; 4.College of Information Engineering, Chengdu University of Technology, Chengdu 610059, China
Abstract:The existence of many high-yielding wells, including X851, X856, X2, X3 and X10, prove the large potential of the Upper Triassic Xujiahe Formation reservoirs in the western Siehuan depression. However, the drilling of several wells with high water production such as CX565 and X201 increase the uncertainty and risk of well emplacement in the study area. There-fore, it is very important to discriminate the gas and water layers in the Xujiahe Formation reservoirs, but difficult to identify a-nomalies of amplitude, frequency and energy in time domain during propagation of waves in the gas and water layers. After seismic signals in time domain are transformed into signals in time-frequency domain by use of the time-frequency analysis meth-od, "low frequency shadow" and "high-frequency attenuation" become significant in gas layers, while they do not occur in wa-ter layers. These unique features of time-frequency domain are used to build up a model for the discrimination of gas and water layers. The results are consistent with the drilling and logging data.
Keywords:Sichuan Basin  west  Late Triassic  tight clastic rock  fluid property  time-frequency  discrimination
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