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Pore-Pressure Prediction in the Permian Basin Using Seismic Prestack Inversion

机译:使用地震灌注倒置的二叠盆盆地的孔隙压力预测

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Although pore pressure is difficult to measure in low permeability rocks such as shale, it nevertheless has an enormous impact on drilling, hydrocarbon production and geomechanics applications such as hydraulic fracturing and wellbore stability analysis. Pore pressure is, thus, a key parameter for economic development of unconventional reservoirs, for which a predrill pore-pressure estimate is essential. In such reservoirs, changes in lithology occur over vertical depth intervals too small to be resolved using seismic velocities derived by means of normal moveout (NMO) analysis or kinematic inversion because these velocities typically have poor vertical resolution. By comparison, inversion of reflection amplitudes yields higher vertical resolution and greater sensitivity to reservoir properties, due to the influence of density in addition to that of velocity. We present an approach for predicting pore pressure based on P-impedance and the ratio V_P/V_S of the vertical P-velocity, V_P, to vertical S-velocity, V_S, obtained from inversion of seismic amplitude variation with offset (AVO) data. Employing P-impedance is analogous to using seismic velocity in conventional seismic-based pore-pressure prediction. However P-impedance from AVO inversion has higher vertical resolution and greater sensitivity than velocities from kinematics. Use of V_P/V_S allows partial compensation for the influence of variable lithology and mineralogy on P-impedance.
机译:尽管孔隙压力难以在低渗透性测量岩石如页岩,它仍然具有上钻孔,烃生产和地质力学应用如水力压裂和井眼稳定性分析产生巨大的影响。孔隙压力,因此,非常规油藏的经济发展,为此,钻前孔隙压力估计是必不可少的一个关键参数。在这样的贮存器,在岩性变化发生在垂直深度间隔太小,使用由正常时差(NMO)分析或运动反转装置衍生因为这些速度通常具有差的垂直分辨率的地震速度来解决。通过比较,反射振幅的产率更高垂直分辨率和更高的灵敏度储层性质,由于密度的除了该速度的影响的反转。我们提出用于预测基于P-阻抗和垂直P-速度的V_P / V_S,V_P比孔隙压力,以垂直的S-速度,V_S,从与偏移(AVO)数据的地震幅度变化的反演得到的方法。使用P-阻抗类似于在常规的基于地震孔隙压力预测使用地震速度。然而从AVO反演P-阻抗具有较高的垂直分辨率和比从运动学的速度更高的灵敏度。 V_P / V_S的使用允许可变岩性和矿物学对P-阻抗的影响的部分补偿。

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