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首页> 外文期刊>Universal Journal of Geoscience >Application of Statics Correction in the Processing of 3D Seismic Data from Onshore Niger Delta
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Application of Statics Correction in the Processing of 3D Seismic Data from Onshore Niger Delta

机译:静力校正在陆上尼日尔三角洲3D地震数据处理中的应用

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Statics correction was applied to a 3D seismic data acquired from an onshore Niger- delta field. The objective of the study was to derive a statics solution, which will correct for time shifts caused by topographic undulations, velocity anomalies in the near-surface and delayed travel times of the reflection signal through the weathered layer. In a previous study by authors, a near-surface seismic velocity and depth model, consisting of the weathering layer and three consolidated (sub-weathering) layers were first estimated. The first-arrivals were picked and used as input for this study. Statics correction consisting of elevation statics, long-wavelength refraction statics, and short-wavelength (residual statics) refraction statics was applied to the data. Interpretation of results show like differences such as a stronger alignment and coherence of reflection events, as well as an upward time shift of the reflection signals when compared with the input data (no statics applied) and the output data (statics applied).
机译:静态校正应用于从尼日尔三角洲陆上油田获取的3D地震数据。该研究的目的是得出一个静态解,它将纠正由地形起伏,近地表速度异常和反射信号穿过风化层的延迟传播时间引起的时移。在作者先前的研究中,首先估计了近地表地震速度和深度模型,该模型由风化层和三个固结(亚风化)层组成。挑选了首批到达的人并将其用作该研究的输入。包括高程静态,长波折射静态和短波(残留静态)折射静态组成的静态校正应用于数据。结果的解释显示出类似的差异,例如与输入数据(未施加静电)和输出数据(已施加静电)相比,反射事件的对齐和相干性更强,以及反射信号的向上时移。

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