Electromagnetic hypogene co-seismic sources
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Publication:2090054
DOI10.1007/978-3-031-05321-4_5zbMath1497.35451OpenAlexW4286619085MaRDI QIDQ2090054
Publication date: 24 October 2022
Full work available at URL: https://doi.org/10.1007/978-3-031-05321-4_5
Seismology (including tsunami modeling), earthquakes (86A15) Inverse problems (including inverse scattering) in optics and electromagnetic theory (78A46) Maxwell equations (35Q61)
Cites Work
- Unnamed Item
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- The quasi-stationary Maxwell equations as singular limit of the complete equations: The quasi-linear case
- Eddy current approximation of Maxwell equations. Theory, algorithms and applications
- A coercive bilinear form for Maxwell's equations
- Hölder regularity for Maxwell's equations under minimal assumptions on the coefficients
- Recovery of a time dependent source from a surface measurement in Maxwell's equations
- Some remarks on a class of inverse problems related to the parabolic approximation to the Maxwell equations: a controllability approach
- An Inverse Source Problem for Maxwell's Equations in Magnetoencephalography
- Inverse source problems for eddy current equations
- Existence and Regularity for Eddy Current System with Nonsmooth Conductivity
- Uniqueness for an inverse problem in electromagnetism with partial data
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