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应用黏弹性波动方程模拟地震低频阴影

Keywords: 低频阴影,地震波衰减,黏弹波动方程,频谱分解

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Abstract:

?以地震频谱分解为基础的低频阴影提取技术是一项有效的烃类检测方法,但是对于低频阴影的产生机理一直缺少明确的解释。本文通过建立含流体饱和介质的等效地质模型,采用黏弹性波动方程进行正演模拟,对得到的合成地震记录进行频谱分解,探讨低频阴影现象的产生机制。在低频(如15hz)瞬时频谱剖面中,含油气储层下方表现为强能量团;当频率增加到55hz以上时,含油气储层下方的能量则比低频瞬时剖面中对应位置的能量要弱得多,这就是典型的低频阴影现象。对低频阴影形成条件的分析结果表明,对于具有低q值(qp小于90,qs小于70)且达到一定厚度(厚度大于半个地震波长)的储层,低频阴影现象明显,出现在储层下方最先存在波阻抗差异的地层界面处。

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