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How Broadband, High Dense, Full Azimuth Point Source Point Receiver Acquisition Improves Seismic Interpretation in Onshore Abu Dhabi

机译:宽带,高密度,完整方位角和点源点接收器采集如何在陆上阿布扎比改善地震解释

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Acquiring seismic data with S4 (Single Source, Single Sensor) is proven technology and it has many advantages over the conventional source and receiver array acquisition type. The array has an intra array statics issue when deployed on large elevation variation such as sand dunes and attenuating higher frequencies as well. S4 with denser spatial sampling with smaller shotline and receiver line spacing could jointly with seismic data broader bandwidth to improve interpreting many seismic details such faults, fractures, tiny stratigraphic features resolution. A debate was raised locally about the value of acquiring seismic data with S4, if only for the sake of acquiring seismic data with shorter time duration compare to the too much equipment needed for array acquisition type that consumes longer time in general. Alternatively, S4 really bring a real value of information and producing an outstanding seismic volume for amenable interpretation with confidence that will lead to utilize the seismic data to help in optimizing the well trajectories placement. This high density broadband 3D seismic acquired survey with fully sampled wave-field data has used the latest acquisition and imaging technologies, it has delivered critical information that can help to reduce drilling risks and to support future 4D reservoir monitoring which improved signal to noise ratio when compared with legacy dataset. An advance seismic processing workflow is tailored to improve the final image quality, and to preserve the azimuthal amplitude variation with offset and azimuth, which in turn can lead to the derivation of intrinsic rock property attributes for better reservoir characterization. A multi azimuth Prestack depth migration approach resolved most of the effects of heterogeneities in the shallow part and in the velocity field, which sometimes can be misinterpreted as azimuthal anisotropy.
机译:通过S4(单源,单个传感器)获取地震数据是经过验证的技术,并且它与传统源和接收器阵列采集类型相比许多优点。当部署在诸如沙丘等大的高程变化上并且也具有衰减较高频率时,该阵列具有帧内阵列静态问题。 S4采用密集空间采样,具有较小的射击线和接收线间距,可以共同利用地震数据更广泛的带宽来改善解释许多地震细节此类故障,裂缝,微小地层特征分辨率。辩论在本地提出关于使用S4获取地震数据的价值,如果仅用于获得较短时间持续时间的地震数据,与阵列采集类型所需的太多设备相比,常规消耗较长的时间。或者,S4真正带来了真正的信息价值,并产生了突出的地震体积,以便充满自信地解释,这将导致利用地震数据来帮助优化井展放置。这种高密度宽带3D地震获取调查采用完全采样的波浪场数据使用了最新的采集和成像技术,它已经提供了有助于减少钻井风险并支持未来的4D水库监测的关键信息,该储层监测改善了信号到噪声比率与传统数据集相比。预先抗震处理工作流程被定制以提高最终的图像质量,并保留带有偏移和方位角的方位传动幅度变化,这又可以导致内在岩石属性的推导,以便更好的储层特征。多方位角普利斯特克深度迁移方法解决了浅层和速度场中异质性的大部分效果,这些速度场有时可以被误解为方位角各向异性。

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