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Barque Pre-SDM - Shallow Initial GeologicalModel Building, and Impact on Deep ReservoirImaging

机译:Barque Pre-SDM - 浅初始地质模型建筑,对深层灌溉的影响

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To de-risk the development of the Barue PH01 extension, there was a need to further improve the qualityof the existing (2000) Pre-SDM imaging. Especially the shallow strata, i.e. the Liassic and the UpperTriassic, demonstrate a strong deformation. During the inversion of the Solepit basin they formed Riedelshears with strongly tilted fault blocks. The impact these dipping strata might have on the Pre-SDMvelocities has been recognised as one of the main causes of the pre-existing imaging uncertainties. Hence,in the new velocity-depth model-building exercise, most attention has been given to the construction of ageologically plausible velocity field for the shallow strata.As tomographic updating based upon RMOonly will most probably not give a satisfactory result due to lack of (shallow) offsets, an initial geologicalmodel has been built using sonic data, seismic dip, faults and paleo-surfaces. This initial model hassubsequently been updated using standard tomographic updating techniques. The final Pre-SDM image,resulting from this procedure, shows a marked improved over earlier depth imaging results; similarly, theexisting TZ-conversion uncertainties have been significantly reduced.
机译:为了使露天PH01延伸的发展,需要进一步提高现有(2000)预测成像的质量。特别是浅层,即Liassic和上层症,表现出强烈的变形。在索入盆地的反转期间,它们形成了具有强烈倾斜的故障块的Riedelshears。这些浸渍地层可能对SDMoCelocities的影响被认为是预先存在的成像不确定性的主要原因之一。因此,在新的速度深度模型建筑锻炼中,大多数人都会对浅层的浅层施工结构的构建。由于缺乏(缺乏),基于额减的严重更新,最可能不会给出令人满意的结果(浅)偏移,使用Sonic Data,地震垂度,断层和古表面建造了初始地质模型。此初始模型使用标准断层摄影更新技术更新了Hassubsem。由此过程产生的最终预先SDM图像显示出在早期深度成像结果上标记的显着改进;同样,The TZ-Conversion不确定性已显着降低。

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