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VSP imaging using free-surface multiples: A case study from the Gulf of Mexico

机译:使用自由表面倍数的VSP成像:来自墨西哥湾的案例研究

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摘要

Vertical seismic profile surveys (VSP) provide a unique opportunity to obtain high-quality seismic images of the subsurface. Placing receivers downhole mitigates many near-surface and overburden challenges associated with surface seismic imaging and results in improved image quality. Unfortunately, these benefits are restricted by the limited area illuminated by the primary P-wave reflection wavefield (typically a relatively narrow cone that underlies the geophone array). The free-surface multiple wavefield recorded in a VSP survey illuminates a significantly larger area, both vertically and laterally, and so can provide an expanded imaging capability (Jiang et al, 2005; Jiang et al, 2007; Lou et al 2007). Subsurface imaging using the multiple wavefield has been demonstrated and is commonly used for imaging deep-water 3D node surveys which are typically acquired using a sparse distribution of receivers. However, no case studies have been published yet which present a critical analysis of the images provided by this technology when applied to VSP surveys.
机译:垂直地震剖面调查(VSP)提供了获得地下优质地震图像的独特机会。将接收器放置在井下可以减轻许多与地表地震成像相关的近地表和覆盖层的挑战,并提高图像质量。不幸的是,这些好处受到初级P波反射波场(通常是在检波器阵列下面的相对较窄的圆锥体)照射的有限区域的限制。 VSP测量中记录的自由表面多波场在垂直和横向上照亮了更大的区域,因此可以提供扩展的成像能力(Jiang等,2005; Jiang等,2007; Lou等2007)。已经证明了使用多重波场的地下成像,并且通常用于成像深水3D节点勘测,这些勘测通常使用接收器的稀疏分布来获取。但是,尚无案例研究发表,该案例研究对应用于VSP调查的此技术提供的图像进行了严格的分析。

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