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A Low Frequency, Passive Seismic Experimentover a Carbonate Reservoir in Abu Dhabi Wavefront and Particle Motion Studi

机译:低频,被动地震实验在阿布扎比波前的碳酸盐储层和粒子运动Studi

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Alow frequency passive seismic experiment conducted over an onshore carbonate oilfield inAbu Dhabiobserved a narrow band of low frequency (2.5 2.8 Hz) signals over both the oil reservoir and the watersaturated zone (Ali et al., 2007). The possible causes of this low frequency energy are not well understoodand it has yet to be demonstrated what types of waves are being observed.In this paper we present results of an investigation carried out to determine the apparent velocities and theazimuth of the wave fronts as well as the particle motion of the recorded low frequency waves.This work is currently ongoing, but the results so far indicates that the observed waves are most likelysome type of surface wave and the azimuth to the source is pointing towards the nearest coastline in thearea (theArabian Gulf).
机译:在陆上碳酸盐油田Inabu Dhabiobserved的频率被动地震实验,在油藏和水库和水坑化区上的低频(2.5 2.8 Hz)信号窄带(Ali等,2007)。这种低频能量的可能原因并不适合理解,尚未显示出观察到的类型的波浪。在本文中我们呈现了对波前方的表观速度和神话的速度和神话的研究结果。也是如此作为记录的低频波的粒子运动。此工作目前正在进行中,但结果到目前为止表明观察到的波是最可能的表面波和源的方位角朝向最近的瑟斯(Thearabian)指向最近的海岸线海湾)。

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