Software for one-dimensional inversion of any frequency EM soundings

Software for one-dimensional inversion of any frequency EM soundings

Tensor-M LLC offers to purchase a program for one-dimensional inversion of frequency electromagnetic sounding data.

Advantages

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Simple and clear user interface
The program is developed for the Windows operating system. The minimalistic single-window interface has all the familiar and intuitive controls for the inversion process. Does not require programming skills.
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Quick results
Computational algorithms are adapted for multiprocessor personal computers for optimal system loading and obtaining the fastest possible results.
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Any field sources
The program supports any type of field source, described by a wire of arbitrary configuration with a three-dimensional position of the nodes. Each wire node can be located at an arbitrary point in the horizontally layered medium and have an arbitrary orientation. When inverting, the completely three-dimensional position of the source is taken into account: horizontal curvilinear, arbitrary inclined (along the topography), partially buried in water or ground.
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Any observation systems
The program supports any observation systems: aero, ground, water, underground and hybrid (for example, the source is on the ground, and the measurements are in the air or underground).
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Determination of electrical resistivity anisotropy. Accounting for displacement currents.
The program allows you to perform anisotropic inversion: automatically determine the horizontal and vertical electrical resistivity for each layer. For high-frequency soundings, taking into account displacement currents (dielectric constant) is relevant. This option is also available to program users.
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Joint inversion
The program allows you to perform joint inversion of data from three types of soundings: frequency EM controlled source soundings, magnetotelluric soundings, direct current soundings. Any combination of the three data types with independent weights is available. For controlled source EM soundings, a combination of an arbitrary set of inverted curves is also available: impedance, tipper, field components. The amplitude and phase weights are set independently.

Proven calculation accuracy in any layer of the model

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    Comparison of the results of calculations of the field of a horizontal electric dipole (HED) located in the ground, obtained in the TENSOR-M 1D and MARE2DEM programs
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    Comparison of the results of calculations of the field of a vertical electric dipole (VED) located in the air, obtained in the TENSOR-M 1D and MARE2DEM programs

    Send your request to purchase a license now: tensorm.llc@gmail.com