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ESTIMATION OF SEISMIC ATTENUATION IN THE KANGAN FORMATION FROM WALKAWAY VSP DATA

机译:从走廊VSP数据估算kangan形成的地震衰减

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In this paper we use the geometry of walkaway vertical seismic profiling (WVSP) in order to define seismic wave attenuation trends in the Kangan reservoir sequences of the South Pars oil field. The mean relative-amplitude attenuation values are analyzed as a function of geophone-source offsets. Our purpose is determining locations in which attenuation shows excessive amounts, that would indicate the possibility if there was any location where there was excessive energy attenuation, that would indicate the possibility of an overpressure zone that would be a drilling hazard. The amplitudes in one walkaway VSP survey line were evaluated to observe any main variation of amplitude in different offsets and to estimate the attenuation of seismic waves energy. Downgoing first arrivals were separated by applying a time window after flattening along a targeted horizon and then performing Fast Fourier Transform (FFT) on first arrivals.In WVSP data acquisition, seismic waves propagate through the geological layers via different source-receiver offsets to reach a constant-geophone depth in subsurface. By processing the amplitudes of these waves, The amounts of attenuation is measured and the lost energy is estimated.
机译:在本文中,我们使用了散游垂直地震剖析(WVSP)的几何形状,以便在南方射口南部康兰储层序列中定义地震波衰减趋势。分析平均相对幅度衰减值作为地震检波器源偏移的函数。我们的目的在于确定衰减显示过多的位置,这将表明如果存在过多的能量衰减的位置,这将表明将成为钻井危害的过压区的可能性。评估一个人走向VSP测量线的幅度,以观察不同偏移中振幅的任何主要变化,并估计地震波能量的衰减。在沿着目标地平线扁平化后应用时间窗口,然后在第一次到达上执行快速傅里叶变换(FFT)后,通过应用快速傅里叶变换(FFT)来分离追溯。在WVSP数据采集时,通过不同的源 - 接收器偏移来通过地质层传播地震波传播恒定的地震孔深度在地下。通过处理这些波的幅度,测量衰减量并估计损失能量。

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