Magnetotelluric frequency division tomography inversion method
A tomographic inversion and magnetotelluric technology, applied in the field of geophysical inversion, can solve problems such as complex steps, achieve the effects of improving resolution, solving low resolution in deep layers, and improving ill-posedness
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[0032] A method for inversion of magnetotelluric frequency division tomography, comprising the following steps:
[0033] Step 1. Estimate effective exploration depth based on observation point frequency data
[0034] The depth reached when most of the energy of the electromagnetic wave (about 63%) is absorbed is called the skin depth, which is estimated by the formula: where ρ is the apparent resistivity, and f is the frequency corresponding to the apparent resistivity. And the depth when the electromagnetic wave energy is attenuated to 50% becomes the effective exploration depth, and its estimation formula is: The effective exploration depth is estimated according to the above formula for all frequency point data of all observation points.
[0035] Step 2. Group the frequency point data:
[0036] Firstly, according to the effective exploration depth and the determined inversion depth, the frequency point data is divided into two groups: the data in the inversion area and...
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