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FULL WAVEFORM INVERSION ON BEKAPAI FIELD: A GAME-CHANGER TECHNOLOGY FOR OUR SEISMIC IMAGING WORKFLOWS

机译:贝卡佩油田的全波形反演:一种用于地震成像工作流程的游戏改变技术

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Seismic imaging of the geological structure of thernBekapai field is challenging. The complex shallowrngeology of the overburden, including fault networksrnin unconsolidated sediments, overshadowed by gasrnclouds, causes several imaging challenges. Largernlateral velocity variations, absorption, shadowingrnzone and push down effects, are hurdles difficult torntackle with conventional depth imaging workflow.rnTotal in-house Full Waveform Inversion technologyrnis addressing some of these challenges. The latestrnhigh-fold long-offset wide-azimuth Ocean BottomrnCable acquisition over the Bekapai field, acquiredrnin 2012, provides a favorable seismic dataset for thernsuccessful application of this technology. FullrnWaveform Inversion is a data-matching waveequation-rnbased tomographic method. The methodrnconstructs a high-resolution velocity model capablernof explaining and characterizing the complex nearsurfacernstructures and properties of the overburden.rnFull Waveform Inversion provides new evidencernwhich reinforces and improves our understanding ofrnthe geology of the Bekapai field. Some of therngeological features, such as relatively thinrncarbonates patches, were already known andrninterpreted on seismic images, but are observed forrnthe first time in a velocity model. The main findingsrnare the extension and thickness of the shallow gasrnanomalies within the gas cloud area, and lowrnvelocity anomalies linked to gas trapped beneathrnshallow normal faults. These latter anomalies werernnever detected before.rnThese low velocities anomalies characterizationrnenables Full Waveform Inversion to resolve somerncomplex image push-downs and concomitantly to improve deeper targets reservoirs imagery. Thernprevious model building methodology which reliedrnon reflection tomography, could not correct forrnthese push-downs. Therefore, Full WaveformrnInversion also constrains the deeper velocity modelrnwhich will be updated by reflection tomography.rnThe integration of Full Waveform Inversion into thernmodel building workflow is the key to its successrnand encourages this approach on similar explorationrnand development projects.
机译:贝恩卡佩地区的地质构造的地震成像具有挑战性。覆盖层复杂的浅层地质学,包括未合并的沉积物的断层网络,被瓦斯云遮盖了,造成了许多成像挑战。传统的深度成像工作流程很难克服较大的横向速度变化,吸收,阴影带和下推效应。内部全全波形反演技术解决了其中一些挑战。 Bekapai油田最新的高倍长偏移宽方位角海底电缆采集于2012年获得,为该技术的成功应用提供了有利的地震数据集。 FullrnWaveform Inversion是一种基于数据匹配波方程的层析成像方法。该方法构造了一个高分辨率的速度模型,能够解释和表征复杂的近地表结构和覆盖层特征。全波形反演提供了新的证据,可以加强和改善我们对Bekapai油田地质的理解。一些地震学特征,例如相对较薄的碳酸盐斑块,已经在地震图像上被已知和解释,但是在速度模型中首次被观察到。主要发现是气云区域内浅层气异常的扩展和厚度,以及与浅层正常断层下陷的瓦斯有关的低速度异常。这些低速异常的特征描述使得全波形反演能够解决一些复杂的图像下探问题,并同时改善深层目标储层的成像效果。依靠反射层析成像的先前的模型构建方法无法校正这些下推式图像。因此,Full WaveformInversion也约束了将通过反射层析成像更新的更深的速度模型。将Full Waveform Inversion集成到模型构建工作流程中是其成功的关键,并鼓励在类似的勘探和开发项目中采用这种方法。

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