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Velocity model building with wave equation migration: the importance of wide azimuth input, versatile tomography, and migration velocity analysis

机译:波动方程迁移的速度模型构建:宽方位角输入,多功能层析成像和迁移速度分析的重要性

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摘要

Wave equation migration is suitable for imaging in complex structures. Ideally, its imaging capability should be matched bycorresponding velocity model building tools. However, the tool of choice for velocity model building, ray-based tomography,at first sight seems weakly compatible with wave equation migration. To overcome this contradiction we propose severalstrategies. The first is to convert the wave equation migration image gathers, typically indexed by subsurface offset, into aformat appropriate for tomography: local reflection angle or its tangent. In conjunction with this conversion, we employa datuming procedure to restrict the tomography to a localized domain where it is compatible with the wave equationmigration band-limited propagation. A second strategy, more expensive and not yet widely tested, is to replace ray-basedtomography with wave-equation-based migration velocity analysis, assuring complete compatibility with the imaging. Inall cases, we notice that having wide-azimuth data makes velocity model building easier, as any chosen subsurface azimuthcontains specular information.
机译:波动方程偏移适用于复杂结构中的成像。理想情况下,其成像能力应通过相应的速度模型构建工具进行匹配。但是,乍一看,用于速度模型构建的首选工具(基于射线的断层扫描)似乎与波动方程偏移不太兼容。为了克服这一矛盾,我们提出了几种策略。第一种是将通常由地下偏移量索引的波动方程偏移图像集转换为适合层析成像的格式:局部反射角或其切线。结合此转换,我们采用基准程序将断层扫描限制在与波动方程迁移带限传播兼容的局部区域。第二种策略是更昂贵且尚未得到广泛测试的策略,是用基于波方程的迁移速度分析代替基于射线的断层扫描,以确保与成像的完全兼容性。在所有情况下,我们都会注意到,拥有宽方位角的数据使速度模型的建立变得更加容易,因为任何选定的地下方位角都包含镜面信息。

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