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    基于一阶速度−应力方程的起伏地表VTI介质逆时偏移

    Reverse time migration of VTI media in undulating surface based on the first-order velocity-stress equation

    • 摘要: 随着油气勘探开发的深入,目标探区呈现复杂地表和复杂构造的双复杂特征,鉴于地表高程变化大和研究重点聚焦于小尺度勘探目标的因素,具有垂直对称轴的横向各向同性(VTI)介质被广泛应用于复杂地质构造的叠前偏移成像中,这些因素都会改变波的传播性质,使得成像方法难以满足高精度成像的需求。为了精确模拟VTI介质的起伏地表下的波场传播特征,将流体力学中的正交贴体网格引入起伏地表下VTI介质的网格剖分中,发展了一套基于起伏地表VTI介质的全交错有限差分模拟算法。并基于正演模拟算法,改进了起伏地表问题下的逆时偏移成像方法。数值模拟结果表明,所发展的模拟方法可以正确模拟起伏地表下VTI介质中的波场传播,并在此基础上进行高精度的RTM成像,成像结果相比于各向同性假设或者规则网格假设下的RTM,更准确地反映了反射面所在的位置,降低了起伏地表对成像结果的影响。

       

      Abstract: As hydrocarbon exploration and development advance, target areas exhibit dual complexities:significant surface elevation variations and a research focus shifting towards smaller-scale targets. Vertically Transverse Isotropic (VTI) media are widely applied in prestack migration imaging for complex geological structures. These factors collectively alter wave propagation characteristics, making existing imaging methods inadequate for current high-precision imaging demands. To accurately simulate wavefield propagation in VTI media beneath rugged topography, the boundary-fitted orthogonal grid concept from fluid dynamics was introduced for discretizing VTI media under irregular surfaces. This led to the development of a fully staggered-grid finite-difference simulation algorithm specifically designed for VTI media with topographic relief. Building upon this forward modeling algorithm, the reverse time migration imaging method was enhanced to address the challenges posed by irregular surfaces. Numerical modeling results demonstrate that the proposed method can correctly simulate wave propagation in VTI media with surface topography and achieve high-precision RTM imaging.compared to RTM results based on isotropic assumptions or regular grid discretizations, the imaging outcomes more accurately reflect reflector positions and exhibit fewer imaging artifacts caused by surface topography.

       

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