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    • 66. 发明公开
    • Method of attenuating coherent noise in marine seismic data
    • 在海洋地震活动中,维尔法赫森zumAbschwächenvon coherentenLärm。
    • EP0681193A1
    • 1995-11-08
    • EP95303020.2
    • 1995-05-03
    • WESTERN ATLAS INTERNATIONAL, INC.
    • Dragoset, William H., Jr.
    • G01V1/36
    • G01V1/36G01V1/364G01V2210/32G01V2210/3246G01V2210/38
    • A method of attenuating coherent environmental noise from a multitrace digitized seismic recording adaptively creates a filter for that attenuation. The method uses the presence, on the recording, of a limited sample of pure noise that is uncontaminated by desired signal. The pure noise sample is used to discover the location of the noise source and from that discovery, to extrapolate and reconstruct the characteristics of the noise envelope as it would appear on the seismic recording. The reconstructed noise envelope is used as a noise reference for input to a conventional iterative adaptive noise cancellation filter loop (24, 28, 30) . For stability, the loop gain is minimized by temporally and spatically averaging the filter coefficients of the loop for each sample interval.
    • 从多雷达数字化地震记录中衰减相干环境噪声的方法自适应地创建用于该衰减的滤波器。 该方法使用在所记录的情况下存在未被所需信号污染的纯噪声的有限样本。 纯噪声样本用于发现噪声源的位置,并从该发现中推断出噪声包络的特征,并将其显现在地震记录上。 重建的噪声包络被用作用于输入到常规迭代自适应噪声消除滤波器环路(24,28,30)的噪声参考。 为了稳定性,通过对每个采样间隔的循环的滤波器系数进行时间和频率平均来最小化环路增益。
    • 67. 发明公开
    • Seismic exploration
    • 地震勘探。
    • EP0674189A2
    • 1995-09-27
    • EP95301995.7
    • 1995-03-24
    • WESTERN ATLAS INTERNATIONAL, INC.
    • Doyen, Philippe M.Psaila, David E.
    • G01V1/28
    • G01V1/30G01V11/00
    • A discretized lithologic model of the subsurface is defined by a regular array of pixels (x). Each pixel (x) corresponds to one of a finite number of possible lithoclasses such as sand, shale or dolomite. The lithoclasses are unknown except at a small number of sparsely distributed control pixels associated with borehole locations. Associated with each pixel there is a multivariate record of seismic attributes that may be statistically correlatable with the local lithology. A Monte Carlo method is used to simulate the lithoclass spatial distribution by combining the lithologic data at control pixels with the seismic-attribute data records. Using Indicator Kriging, a prior probability distribution of the lithoclasses is calculated for each pixel from the lithology values at neighboring pixels. The likelihood of each lithoclass is also calculated in each pixel from the corresponding conditional probability distribution of seismic attributes. A posterior lithoclass probability distribution is obtained at each pixel by multiplying the prior distribution and the likelihood function. The posterior distributions are sampled pixel-by-pixel to generate equally probable models of the subsurface lithology.
    • 用于通过将对应于井位置的多个分布式控制像素的已知岩性数据与从与像素相关联的站收集的地震属性组合而在常规像素阵列上产生离散岩石类值的模拟模型的方法包括:(a)测量物体 几个地层的性质; (b)计算每个岩石类的地震属性的条件概率分布; (c)随机选择尚未被模拟的像素; (d)通过组合附近的控制像素处的岩性数据来估计所选择的像素处的岩石类的先验概率分布函数; (e)根据地震属性的岩石类条件分布计算所选像素中的岩石类似然函数; (f)通过将先验分布函数与似然函数组合来计算所选像素中的光刻胶的后验分布函数; (g)通过从后验概率分布函数中随机采样来绘制所选像素中的模拟岩石类阀; (h)作为附加的控制像素将模拟的光刻类值输入到阵列中; (i)重复步骤(b)至(g),直到对阵列的所有像素模拟岩石类值; 和(j)产生地球地下的岩性模型。