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首页> 外文期刊>The Leading Edge >Over/under towed-streamer acquisition: A method to extend seismic bandwidth to both higher and lower frequencies
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Over/under towed-streamer acquisition: A method to extend seismic bandwidth to both higher and lower frequencies

机译:拖缆上方/下方采集:一种将地震带宽扩展到较高和较低频率的方法

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摘要

Seismic resolution of towed marine-streamer data is affected by free-surface reflections. They strongly modulate the spectrum reducing energy at the so-called notch frequencies, f_n = iv/2z {i = 0,1,...,∞}, in which v is the water velocity and z is the source or receiver depth. As a result there is a very strong loss of useful low-frequency energy and usually a similar loss at higher frequencies. The ghost effect occurs both at the source and at the receiver. At the source, the upgo-ing part of the source wavefield is reflected off the free surface with inverted polarity before its delayed journey into the Earth. At the receiver, the upgo-ing part of the receiver wavefield is reflected off the free surface with inverted polarity before it travels down to the receiver again. The over/under acquisition method allows separation of the up- and downgoing wavefields at the source (or receiver) using a vertical pair of sources (or receivers) to determine wave direction. In this article, we present the results of two experiments conducted in the Gulf of Mexico in 2004 and 2006 to investigate the use of over/under sources and receivers.
机译:拖曳的海上拖缆数据的地震分辨率受自由表面反射的影响。它们在所谓的陷波频率f_n = iv / 2z {i = 0,1,...,∞}处强烈调制频谱降低能量,其中v是水速,z是源或接收器深度。结果,有用的低频能量会非常强烈地损失,而在高频处通常会损失相似的损失。重影效应在源和接收器处均发生。在源头,源波场的上行部分在其延迟进入地球之前被极性反转的自由表面反射。在接收器处,接收器波场的上行部分以相反的极性从自由表面反射,然后再次向下传播到接收器。过高/欠采集方法允许使用垂直的一对源(或接收器)在源(或接收器)处分离上行和下行波场,以确定波的方向。在本文中,我们介绍了2004年和2006年在墨西哥湾进行的两个实验的结果,以调查过度/不足信号源和接收器的使用。

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