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Geohazard Detection in Deepwater Clastics Basins Using a Seismic Technique Guided by Geology and Rock Physics Model: Methodology and Examples

机译:地质和岩石物理模型指导下的地震技术在深水碎屑岩盆地的地质灾害探测:方法和实例

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Detection of hazardous zones, associated with high-pressuredrnfluids in unconsolidated sands and shales, prior to drilling, isrnessential for environmental as well as health and safety.rnDrilling for deepwater targets is associated with high cost andrnrisk, while margins of commercial operations are small.rnTherefore, it is imperative to control cost through accuraternwell planning and reliable anticipation of geohazards.rnThis paper deals with a novel seismic approach that usesrnthe full bandwidth and the entire offset range of the conventionalrn3D seismic data to detect the presence of hazardousrnzones. Both in shallow and deeper zones, P- and S-velocitiesrnare determined using seismic full waveform prestack inversion.rnShallow water flow (SWF) layers in the deepwater arernidentified through the associated high ratios of P- to Svelocities.rnA new, rock model-based approach especiallyrnsuited for deepwater pore pressure imaging was appliedrnto predict the presence of both shallow and deeperrnover-pressured zones.rnThis paper covers the essential elements of the workflow –rna “five-step process” for hazard identification that integrates arnspecial data processing flow with prestack and full waveformrninversion of 3D seismic data with geology and rock modelsrnappropriate for shallow water flow, gas hydrates and deeperrngeohazards. Real data examples from deepwater elucidaternthe approach.
机译:在钻探之前发现与未固结的砂岩和页岩中的高压流体有关的危险区域,对环境以及健康和安全都是至关重要的因此,必须通过准确的井眼计划和可靠的地质灾害预测来控制成本。本文涉及一种新颖的地震方法,该方法利用常规3D地震数据的全部带宽和整个偏移范围来检测危险区域的存在。无论是在浅层还是深层,都使用地震全波叠前反演来确定P和S速度.rn通过相关的P与速度的高比率来识别深水中的浅水流(SWF)层。本文采用了特别适合深水孔隙压力成像的方法来预测浅压区和深压区的存在。本文涵盖了工作流程的基本要素–用于危害识别的“五步法”,该方法将专业数据处理流程与叠前和后处理集成在一起。具有地质和岩石模型的3D地震数据的全波形反演适用于浅水流动,天然气水合物和深部地质灾害。实际数据示例来自深水解析方法。

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