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Advanced seismic processing/imaging techniques and their potential for geothermal exploration

机译:先进的地震处理/成像技术及其在地热勘探中的潜力

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Seismic reflection imaging is a geophysical method that provides greater resolution at depth than other methods and is, therefore, the method of choice for hydrocarbon-reservoir exploration. However, seismic imaging has only sparingly been used to explore and monitor geothermal reservoirs. Yet, detailed images of reservoirs are an essential prerequisite to assess the feasibility of geothermal projects and to reduce the risk associated with expensive drilling programs. The vast experience of hydrocarbon seismic imaging has much to offer in illuminating the route toward improved seismic exploration of geothermal reservoirs ——but adaptations to the geothermal problem are required. Specialized seismic acquisition and processing techniques with significant potential for the geothermal case are the use of 3D arrays and multicomponent sensors, coupled with sophisticated processing, including seismic attribute analysis, polarization filtering/migration, converted-wave processing, and the analysis of the diffracted wavefield. Furthermore, full-waveform inversion and S-wave splitting investigations potentially provide quantitative estimates of elastic parameters, from which it may be possible to infer critical geothermal properties, such as porosity and temperature.
机译:地震反射成像是一种地球物理方法,在深度上比其他方法具有更高的分辨率,因此是油气藏勘探的首选方法。但是,地震成像仅很少用于勘探和监测地热储层。然而,详细的储层图像是评估地热项目可行性并降低与昂贵的钻井计划相关的风险的基本前提。碳氢化合物地震成像的丰富经验可为阐明改进地热储层地震勘探的途径提供很多信息,但需要适应地热问题。具有地热潜力的特殊地震采集和处理技术是3D阵列和多分量传感器的使用,结合复杂的处理功能,包括地震属性分析,极化滤波/迁移,转换波处理以及衍射波场分析。此外,全波形反演和S波分裂研究潜在地提供了弹性参数的定量估计,从中可以推断出关键的地热性质,例如孔隙度和温度。

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