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Exploring multiple 3D inversion scenarios for enhanced interpretation of marine CSEM data: an iterative migration analysis of the Shtokman gas field

机译:探索多种3D反演场景以增强对海洋CSEM数据的解释:Shtokman气田的迭代运移分析

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摘要

The premise of the various marine controlled-sourceelectromagnetic (CSEM) methods is sensitivity tothe lateral extents and thicknesses of resistive bodiesembedded in conductive hosts. For this reason, CSEMmethods were initially applied to de-risking exploration andappraisal with direct hydrocarbon indication. However,CSEM methods represent just part of an integrated explora-tion strategy. The value of CSEM data is only realizedwhen it is integrated with sound geological understandingin a shared earth model. The most successful applicationsof CSEM to date have been in complement to those seis-mic interpretations where lithological or fluid variationscannot be adequately discriminated by seismic methodsalone (Hesthammer et al. 2010). Methods for interpretingCSEM data are complicated by the very small responses ofhydrocarbon-bearing reservoir units when compared to thetotal fields. CSEM interpretation is inherently reliant oniterative inversion methods since the data cannot simply beseparated or transformed with linear operators as per seismicmethods.
机译:各种海洋可控源电磁(CSEM)方法的前提是对嵌入导电主体中的电阻体的横向范围和厚度敏感。由于这个原因,CSEM方法最初被用于具有直接碳氢化合物指示的低风险勘探和评估。但是,CSEM方法仅代表集成勘探策略的一部分。 CSEM数据的价值只有在将其与合理的地质认识结合到一个共享的地球模型中时才能实现。迄今为止,CSEM的最成功应用是对地震学解释的补充,在这些地震学解释中,仅靠地震方法无法充分区分岩性或流体变化(Hesthammer等人,2010)。与总油田相比,含烃储层单元的响应非常小,因此解释CSEM数据的方法非常复杂。 CSEM解释固有地依赖于迭代反演方法,因为无法根据地震方法简单地使用线性算子对数据进行分离或转换。

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