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3-D SEISMIC REFLECTION TOMOGRAPHY ON TOP OF THE GOCAD DEPTH MODELER

机译:GOCAD深度建模器顶部的3D地震反射层析成像

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The estimation of velocity macro-models by seismic reflection tomography is studied in three-dimensions. Inversion techniques based on the kinematics of seismic data require an appropriate parameterization of the geological macro-model, in particular as far as the velocity field is concerned. The step toward structurally complex geological models is achieved by exploiting a new approach to 3-D depth modeling: GOCAD. The peculiarities inherent to GOCAD triangulated surfaces and its associated discrete smooth interpolator (DSI) have led to the development of original ray-tracing techniques. By exploiting intensively the topology of the triangulated surfaces, these new algorithms make it possible to reach a good balance between accuracy and computation performance. To build a 3-D macro-model estimation tool, ray-tracing is then associated with a least-squares inversion of depth parameters and velocity parameters from 3-D zero-offset traveltimes and stacking velocities, or multi-offset prestack traveltimes from 2-D seismic lines. [References: 25]
机译:研究了三维地震反射层析成像对速度宏模型的估计。基于地震数据运动学的反演技术需要对地质宏模型进行适当的参数化,特别是在涉及速度场方面。通过开发3-D深度建模的新方法GOCAD,可以实现结构复杂的地质模型。 GOCAD三角表面及其相关的离散平滑插值器(DSI)固有的特性导致了原始射线跟踪技术的发展。通过集中利用三角化表面的拓扑,这些新算法使在精度和计算性能之间达到良好的平衡成为可能。要构建3-D宏模型估计工具,然后将光线跟踪与3-D零偏移行进时间和堆叠速度的深度参数和速度参数的最小二乘反演关联,或者将2的多偏移叠前行进时间与-D地震线。 [参考:25]

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