多分量偏置VSP比例模型研究

D.R Pant, S.A Greenhalgh
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引用次数: 4

摘要

提高地下地震构造知识的关键在于多分量记录(多向震源和三轴探测)和矢量(弹性)波场成像的使用。为此,我们组装了一个二维双轴物理地震模型系统。该实验室设备已用于在一个非常简单的反射结构上获取VSP和MSP(倒VSP)阵列配置的矢量地震数据。控制方向接收(CDR)滤波得到上行P波、下行P波、上行S波和下行P波四个剖面进行解释。模型实验揭示了瑞利波(或管波,推广到现场)向散射S波的有趣模式转换,并在地震剖面中占主导地位。这种波在标量地震图上可能是一种麻烦的噪声形式,但它可以通过CDR消除,只通过P波。或者,它可以被视为一种有用的多分量诊断方法,用于检测裂缝或其他与井眼相交的阻抗边界。
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A multicomponent offset VSP scale model investigation

The key to obtaining improved knowledge of the subsurface seismic structure lies in the use of multicomponent recording (multi-directional sources and triaxial detection) and vector (elastic) wavefield imaging. To this end we have assembled a two-dimensional, biaxial physical seismic model system.

The laboratory facility has been used to acquire vector seismic data over a very simple reflecting structure for both VSP and MSP (inverted VSP) array configurations. Controlled direction reception (CDR) filtering of the data yields four sections for interpretation: upgoing P, downgoing P, upgoing S and downgoing S.

The model experiment has revealed an interesting mode conversion from Rayleigh wave (or tube wave, when extended to the field situation) to scattered S wave, which dominates the seismic section. This wave could be a troublesome form of noise on scalar seismograms, but it can be eliminated by means of CDR to pass the P waves only. Alternatively, it can be viewed as a useful multicomponent diagnostic for detecting fractures or other impedance boundaries intersecting the borehole.

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