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Method and Results of Estimating Acoustic Characteristics of Bottom-Sediment Upper Layers in the Shelf Region Using Seismic Exploration Instruments

机译:地震勘探仪器估算架子区底泥上层声学特征的方法和结果

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摘要

The potential of seismic exploration instruments for estimating the surface layers of soil in the towing zone of an extended multielement array is investigated. In contrast to the well-known method of common depth point, in which the main estimated parameters are the transit times of waves reflected from deep layers of the sea bottom, two-dimensional spectral analysis is used to measure the longitudinal wavenumbers of the modes forming an infrasonic field in the water layer. The measured longitudinal wavenumbers of modes serve initial data for estimating the acoustic characteristics of the upper layers of bottom sediments directly in the towing zone of pulse emitter and extended multielement array. It is concluded that the use of data on the parameters of upper soil layers in seismic exploration should increase the accuracy of contouring oil and gas condensate fields.
机译:研究了地震勘探仪器在扩展多元素阵列牵引带中估算土壤表层的潜力。与众所周知的常用深度点方法(主要估算参数是从海底深层反射的波的传播时间)相反,二维光谱分析用于测量形成波模的纵向波数。水层中的次声场。测得的模态纵向波数可作为初始数据,用于直接估算脉冲发射器和扩展多元素阵列的牵引带中底部沉积物上层的声学特性。结论是,在地震勘探中使用上层土层参数数据可以提高轮廓油气凝结层的精度。

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