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起伏地形的2.5维主轴各向异性海洋CSEM反演研究

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笔者利用OCCAM方法实现了MPI并行的2.5维海洋CSEM反演算法.正演采用基于非结构网格的有限元方法,在精确模拟海底起伏地形和构造模型的同时,对核心区域和扩展区域进行不同尺度的剖分以减少反演参数.水平海床和起伏海床的理论模型算例表明,沿测线发射的2.5维剖面数据对垂直各向异性模型的恢复效果优于水平各向异性模型.复杂海底地形模型的试算结果表明,带地形沉积层的存在会对反演结果产生较大影响,在实际资料解释中应该引起重视.
Research on 2.5-dimensional axially anisotropy marine CSEM inversion of undulating topography
An MPI parallel 2.5-dimensional marine CSEM inversion algorithm was implemented using the OCCAM meth-od.The forward modeling adopts a finite element method based on unstructured grids,which accurately simulates the seabed's undulating topography and structural model while meshing the core and extended regions at different scales to reduce inversion parameters.The examples of horizontal and undulating seabed models indicate that the recovery effect of the vertical anisotrop-ic model is better than that of the horizontal anisotropic model using 2.5-dimensional profile data emitted along the survey line.The trial results of complex seabed topography models indicate that the presence of sedimentary layers with topography can sig-nificantly impact the inversion results,which should be taken seriously in actual data interpretation.

marine controlled source electromagneticundulating topographyinversionanisotropy

覃金生

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东华理工大学地球物理与测控技术学院,南昌 330013

海洋可控源电磁 起伏地形 反演 各向异性

2024

物探化探计算技术
成都理工大学 中国地质科学院物化探研究所

物探化探计算技术

CSTPCD
影响因子:0.398
ISSN:1001-1749
年,卷(期):2024.46(2)
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