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GEOLOGIC QUALITY FACTOR INVERSION METHOD

机译:地质质量因子反演方法

摘要

Provided is a method for performing layer Q factor inversion by using an amplitude spectrum attribute of a downlink wave of vertical seismic profile data in a geophysical exploration data processing technology. In the method, first an F-K (frequency-wave number) method is used to perform wave field separation on VSP original data, so as to obtain a downlink wave; a downlink sub-wave and a monitoring sub-wave are selected to undergone Fourier transform to obtain an amplitude spectrum, polynomial fitting is performed on the amplitude spectrum to obtain an equivalent Q, and a formula between the equivalent Q and a layer Q is used to perform inversion, so as to obtain the layer Q. The method has a strong capability of resisting random disturbance, and is capable of removing a difference of triggering sub-wave. The algorithm is simple and can greatly save workload; moreover, the layer Q value obtained through inversion has a desirable stability and high precision.
机译:提供了一种在地球物理勘探数据处理技术中利用垂直地震剖面数据的下行波的振幅谱属性进行Q层因子反演的方法。该方法中,首先采用F-K(频数)方法对VSP原始数据进行波场分离,得到下行波。选择下行子波和监测子波进行傅立叶变换,得到振幅谱,对振幅谱进行多项式拟合,得到等效Q,并使用等效Q与层Q之间的公式该方法具有很强的抵抗随机干扰的能力,并且能够消除触发子波的差异。该算法简单,可以大大节省工作量;此外,通过反演获得的层Q值具有期望的稳定性和高精度。

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