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    • 56. 发明公开
    • Spatial de-aliasing of the 3-D Kirchhoff DMO operator
    • 在3-D Kirchhoff DMO操作员中的Beseitigung von Aliasing
    • EP0869375A2
    • 1998-10-07
    • EP98302529.7
    • 1998-04-01
    • WESTERN ATLAS INTERNATIONAL, INC.
    • Beasley, Craig J.Mobley, Everett C.
    • G01V1/36
    • G01V1/362G01V2210/522
    • A method is disclosed for processing seismic survey data to generate an unaliased 3-D DMO operator using two dimensional sampling theory to the spatial traverse of the operator as well as to the temporal axis. First a continuous DMO operator is generated along the line segment (10) connecting a source (5) and a receiver (R) directed at an arbitrary azimuth relative to a biaxial output grid. The operator is discretized at spaced-apart sample points (such as 16,18,20,30) along the DMO aperture segment (10), the spacing (D) being equal to or less than the output grid dimensions (dx,dy). An exponentially tapered sinc filter function is applied to the samples which are then interpolated onto the output grid.
    • 公开了一种用于处理地震勘测数据以产生使用二维采样理论对操作者的空间横移以及到时间轴的未混叠的三维DMO算子的方法。 首先,沿着连接相对于双轴输出栅格的任意方位角的源(5)和接收器(R)的线段(10)生成连续的DMO操作器。 操作者沿着DMO孔径段(10)在间隔开的采样点(例如16,18,20,30)处离散,间隔(D)等于或小于输出栅格尺寸(dx,dy) 。 将一个指数渐变的sinc滤波函数应用于样本,然后插值到输出栅格上。
    • 57. 发明公开
    • Measuring sea floor reflectivity
    • 测量海底反射率
    • EP0851243A2
    • 1998-07-01
    • EP97310219.7
    • 1997-12-17
    • WESTERN ATLAS INTERNATIONAL, INC.
    • Paffenholz, Josef
    • G01V1/38G01H15/00
    • G01V1/38G01V1/28G01V2210/56
    • The two-way water-layer travel time, τ, is derived from dual-mode seismic sensor data by cross-correlating the Fourier transforms of the sum and difference of the velocity and pressure signatures. The Z-transform of τ evaluates one of the two Backus variables, Z w . The second variable is R b , the water bottom reflectivity coefficient. The frequency-domain transforms of the above summed and differenced signatures are each multiplied by the Backus operator (1+R b Z w ) 2 after initializing R b and the products are iteratively cross-correlated until the correlation function converges to a minimum. R b is perturbed after each iteration. The value of R b upon convergence is the local water bottom reflectivity coefficient.
    • 双向水层传播时间τ是通过对速度和压力特征的和与差的傅立叶变换进行互相关而从双模式地震传感器数据导出的。 τ的Z变换评估两个Backus变量之一Zw。 第二个变量是Rb,即水底反射系数。 在初始化Rb之后,上述总和和差异签名的频域变换各自乘以Backus算子(1 + RbZw)2,并且产品迭代交叉相关,直到相关函数收敛到最小。 每次迭代后Rb都会受到干扰。 收敛时Rb的值是局部水底反射系数。