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Accuracy of wavelets, seismic inversion, and thin-bed resolution

机译:小波,地震反转和薄层分辨率的精度

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Broadband reprocessed seismic data from the North West Shelf of Australia were inverted using wavelets estimated with a conventional approach. The inversion method applied was a facies-based inversion, in which the low-frequency model is a product of the inversion process itself, constrained by facies-dependent input trends, the resultant facies distribution, and the match to the seismic. The results identified the presence of a gas reservoir that had recently been confirmed through drilling. The reservoir is thin, with up to 15 ms of maximum thickness. The bandwidth of the seismic data is approximately 5-70 Hz, and the well data used to extract the wavelet used in the inversion are only 400 ms long. As such, there was little control on the lowest frequencies of the wavelet. Different wavelets were subsequently estimated using a variety of new techniques that attempt to address the limitations of short well-log segments and low-frequency seismic. The revised inversion showed greater gas-sand continuity and an extension of the reservoir at one flank. Noise-free synthetic examples indicate that thin-bed delineation can depend on the accuracy of the low-frequency content of the wavelets used for inversion. Underestimation of the low-frequency contents can result in missing thin beds, whereas underestimation of high frequencies can introduce false thin beds. Therefore, it is very important to correctly capture the full frequency content of the seismic data in terms of the amplitude and phase spectra of the estimated wavelets, which subsequently leads to a more accurate thin-bed reservoir characterization through inversion.
机译:澳大利亚西北架子的宽带再加工地震数据使用以传统方法估计的小波反转。应用的反演方法是基于相的反转,其中低频模型是反演过程本身的乘积,受相位依赖的输入趋势约束,所得相片分布和与地震匹配的匹配。结果确定了最近通过钻井确认的气体储层的存在。储存器薄,最大厚度高达15毫秒。地震数据的带宽约为5-70Hz,并且用于提取在反转中使用的小波的井数据长度仅为400毫秒。因此,对小波的最低频率几乎没有控制。随后使用各种新技术估计不同的小波,该技术试图解决短良好的对数段和低频地震的局限性。修订后的反演显示出更大的气砂连续性和储层在一个侧翼的延伸。无噪音合成实例表明薄床描绘可以取决于用于反转的小波的低频含量的精度。低估低频内容会导致缺失的薄床,而低频率低估可以引入假薄床。因此,根据估计小波的幅度和相位谱来正确地捕获地震数据的全频率内容非常重要,这随后通过反转导致更精确的薄床储存器。

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