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Seismic imaging of thrust faults and structural damage: a visualization workflow for deepwater thrust belts

机译:推力断层和结构破坏的地震成像:深水推力带的可视化工作流程

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摘要

Combinations of increasingly sophisticated software and hardware have greatly improved the imaging of geologic structure and stratigraphic features in seismic datasets (Marfurt and Chopra, 2007). Today the seismic interpreter can quickly create attribute maps, using specific filtering workflows to identify, visualize, and isolate faults and fracture systems at different scales. Such techniques have been successfully applied for imaging normal faults (Dutzer et al., 2009) within reservoirs associated with extensional sedimentary basins (Chopra and Marfurt, 2007). However, most of the adopted interpretation strategies assume fault structures to be rather simple – represented as narrow curvi-planar surfaces that transect the seismic data.
机译:日益复杂的软件和硬件的组合极大地改善了地震数据集中的地质结构和地层特征的成像(Marfurt和Chopra,2007)。如今,地震解释器可以使用特定的过滤工作流程来快速创建属性图,以识别,可视化和隔离不同规模的断层和断裂系统。此类技术已成功地用于对与伸展沉积盆地有关的储层中的正常断层成像(Dutzer等,2009)(Chopra和Marfurt,2007)。但是,大多数采用的解释策略都假定断层结构相当简单-表示为横切地震数据的狭窄曲线平面。

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