Inversion of low-frequency subsurface data in a finite-depth ocean
نویسندگان
چکیده
منابع مشابه
improving the inversion of helicopter-borne frequency-domain electromagnetic data with depth constrained
generally, the measured secondary field data is inverted into resistivity using two principal models; the homogeneous half-space model and the layered half-space model. while the homogeneous half-space inversion uses single frequency data, the inversion is done individually for each of the frequencies used, the multi-layer 1d inversion is able to take the data of all frequencies available into ...
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Discrimination of the blind and dispersed mineralization deposits is a challenging problem in geochemical exploration. The frequency domain (FD) of the surface geochemical data can solve this important issue. This new exploratory information can be achieved using the interpretation of FD of geochemical data, which is impossible in spatial domain. In this research work, FD of the surface geochem...
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APPROACH Consider the simulated SW06 scenario with a “true” bottom consisting of 3 sediment layers (to taling 22m in depth extent – a medium thickness) where all three sediment layers are each defined by a linear sound-speed profile (and constant densities) all over a half-space (constant sound-speed and density) as seen in Fig. 1. For the inversion processing we shall (as in earlier work) ass...
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ژورنال
عنوان ژورنال: Applied Mathematics Letters
سال: 1994
ISSN: 0893-9659
DOI: 10.1016/0893-9659(94)90044-2