Process / pipelineParameter recovery
地球物理反演
地球物理反演是利用观测到的地球物理数据来估计地下性质和结构的过程。该数学框架由Tikhonov（1963）形式化，由Tarantola（1987）扩展，解决了反演问题：给定测量值（重力、磁力、地震、电法），是哪种地下模型产生了它们？反演是所有定量地球物理学的核心，能够从地表或钻孔测量中提取详细的地下信息。
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来源
- Tarantola, A. (1987). Inverse Problem Theory: Methods for Data Fitting and Model Parameter Estimation. Elsevier. link ↗
- Constable, S. C., Parker, R. L., & Constable, C. G. (1990). Occam's inversion: A practical algorithm for generating smooth models from electromagnetic sounding data. Geophysics, 55(3), 289–300. link ↗
- Menke, W. (2012). Geophysical Data Analysis: Discrete Inverse Theory (3rd ed.). Academic Press. link ↗
如何引用本页
ScholarGate. (2026, June 3). Geophysical Inversion. ScholarGate. https://scholargate.app/zh/geoscience/geophysical-inversion
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