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Application of multiparameter full-waveform inversion in Central Luconia Basin, Sarawak

机译:多参数全波形反演在砂拉越中卢卡尼亚盆地的应用

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摘要

Reducing velocity inaccuracy in complex settings is of paramount importance for limiting structural uncertainties, therefore helping the geologic interpretation and reservoir characterization. Shallow velocity variations due, for instance, to gas accumulations or carbonate reefs, are a common issue offshore Malaysia. These velocity variations are difficult to image through standard reflection-based velocity model building. We have applied full-waveform inversion (FWI) to better characterize the upper part of the earth model for a shallow-water field, located in the Central Luconia Basin offshore Sarawak. We have inverted a narrow-azimuth data set with a maximum inline offset of 4.4 km. Thanks to dedicated broadband preprocessing of the data set, we could enhance the signal-to-noise ratio in the 2.5-10 Hz frequency band. We then applied a multiparameter FWI to estimate the background normal moveout velocity and the η-parameter. Full-waveform inversion together with broadband data processing has helped to better define the faults and resolve the thin layers in the shallow clastic section. The improvements in the velocity model brought by FWI lead to an improved image of the structural closure and flanks. Moreover, the increased velocity resolution helps in distinguishing between two different geologic interpretations.
机译:减少复杂环境中的速度误差对于限制结构不确定性至关重要,因此有助于地质解释和储层表征。例如,由于天然气聚集或碳酸盐岩礁造成的浅层速度变化是马来西亚近海的常见问题。这些速度变化很难通过基于标准反射的速度模型构建来成像。我们已经应用了全波形反演(FWI)来更好地表征位于砂拉越近海卢中盆地中部的浅水场的地球模型的上部。我们反转了一个最大方位偏移为4.4 km的窄方位角数据集。由于对数据集进行了专用的宽带预处理,因此我们可以提高2.5-10 Hz频带中的信噪比。然后,我们应用多参数FWI来估计背景法向运动速度和η参数。全波形反演与宽带数据处理一起有助于更好地确定断层并解决浅碎屑岩层中的薄层。 FWI带来的速度模型的改进导致结构封闭和侧面的图像得到改善。此外,提高的速度分辨率有助于区分两种不同的地质解释。

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