A Multipolar Magnetotelluric Sounding Method

Abstract

The invention discloses a multi-polarization magnetotelluric sounding method, which includes setting a plurality of pairs of electrodes along the direction of the survey line and perpendicular to the survey line and observing the electric field in the x and y directions on each survey point with the survey point as the center; Set up magnetic rods in the x direction of the survey line and the y direction of the vertical survey line and observe the magnetic fields in the x and y directions; simultaneously observe the multi-pole distance electric field and magnetic field and obtain the measured time series of the magnetic field and the measured time series of the electric field; the measured time series of the magnetic field and The electric field measured time series is processed for data processing to complete the common-point, same-frequency, multi-polarization magnetotelluric sounding. The multi-polarization magnetotelluric sounding method provided by the present invention can detect multi-electrode distances at the same point and frequency, and can weaken the static effect caused by surface inhomogeneity through data processing, and improve the detection of complex and irregular three-dimensional geological bodies precision, and the method of the present invention has high reliability, is simple and convenient.

Description

technical field [0001] The invention belongs to the field of geophysical exploration, and in particular relates to a multi-polarization magnetotelluric sounding method. Background technique [0002] Tichonov in 1950 and Cagnaird in 1953 proposed the magnetotelluric method (MT) based on the theory of plane electromagnetic waves, and gradually developed the audio-frequency magnetotelluric method (AMT) and controllable Source audio magnetotelluric sounding (CSAMT), collectively referred to as plane wave magnetotelluric sounding, these methods are widely used in the field of geological exploration. At present, the observation methods based on the plane wave electromagnetic sounding method can be divided into the following types: 1. Scalar mode, observe a set of horizontally orthogonally polarized electric and magnetic fields; 2. Vector mode, observe two groups of horizontally orthogonally polarized Electric field and magnetic field; 3. Tensor mode, not only to observe two sets ...

AI Technical Summary

Problems solved by technology

However, the underground medium is a complex three-dimensional geological body, and one electric field pitch cannot completely describe the electromagnetic multi-polarization response characteristics of the complex and irregular three-dimensional geological body underground (such as figure 1 shown)

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