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海洋可控源电磁法与地震全波形二维联合反演研究

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为降低单一地球物理反演方法的局限性以及反演中所存在的多解性等问题,开展了海洋可控源电磁法(MCSEM)与地震全波形的二维联合反演研究.MCSEM采用数据空间OCCAM反演算法,地震全波形采用梯度法反演算法,引入交叉梯度函数实现两种物性参数结果的相互耦合;开发出一套二维联合反演算法,并通过 3 组理论模型算例验证了算法的准确性.研究结果表明:MCSEM联合反演结果相对于单方法反演结果有显著改善和提升,主要体现在异常体的形态刻画、结构构造以及物性数值的恢复,这说明全波形的反演方法能够提高MCSEM反演结果的可靠性.
Two-dimensional joint inversion based on the marine controlled-source electromagnetic method and seismic full-waveform
To reduce the limitations and the multiplicity of solutions of a single geophysical inversion method,this study investigated the two-dimensional joint inversion based on the marine controlled-source electromagnetic(MCSEM)method and seismic full-waveform inversion.The MCSEM method employs the data-space Occam's algorithm,while the seismic full-waveform inversion utilizes the gra-dient algorithm.By incorporating a cross-gradient function for the mutual coupling of the two types of physical property parameters,this study developed a two-dimensional joint inversion method,whose accuracy was verified using three different models.As indicated by the results,compared to a single inversion method,the MCSEM-based joint inversion yielded significantly improved inversion results,predominantly in terms of the morphology characterization of anomalous bodies,as well as the reconstruction of their structure and tex-tures and their physical property values.Therefore,the full-waveform inversion can enhance the reliability of the MCSEM inversion re-sults.

marine controlled-source electromagnetic(MCSEM)seismic full-waveformcross-gradientjoint inversion

孔繁祥、谭捍东、刘建勋

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中国地质科学院 地球物理地球化学勘查研究所,河北 廊坊 065000

中国地质大学(北京)地球物理与信息技术学院,北京 100083

海洋可控源电磁法 地震全波形 交叉梯度 联合反演

中国地质调查局地质调查项目中国地质科学院地球物理地球化学勘查研究所所长基金基本科研业务费项目

DD20230298A2022P02

2024

物探与化探
中国国土资源航空物探遥感中心

物探与化探

CSTPCD
影响因子:0.828
ISSN:1000-8918
年,卷(期):2024.48(1)
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