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Magnetotellurics

open access: yes, 2007
Martyn Unsworth
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Magnetotelluric exploration for hydrocarbons

Proceedings of the IEEE, 1989
The magnetotelluric (MT) method utilizes naturally occurring low-frequency electromagnetic energy to determine the electrical resistivity of the Earth's subsurface. The resistivity distribution of the subsurface is then interpreted in terms of rock type and geologic structure.
openaire   +1 more source

MTpy: A Python toolbox for magnetotellurics

Computers & Geosciences, 2014
We present the software package MTpy that allows handling, processing, and imaging of magnetotelluric (MT) data sets. Written in Python, the code is open source, containing sub-packages and modules for various tasks within the standard MT data processing and handling scheme.
Lars Krieger, Jared R. Peacock
openaire   +3 more sources

Directional noise cancelling in magnetotellurics

55th EAEG Meeting, 1993
In Magnetotelluric (MT) data processing, poor signal-to-noire ratio usually biaces the impedance tensor Z elements estimates. Strong electromagnetic (EM) noise may thus render the MT method impracticable in industrial areas. Noise due to periodic sources (i.e. power line harmonies) is easily removed by analog filtering in the field; but non-periodic EM
Spagnolini, U., Santarato, G.
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The Magnetotelluric Method

2012
The magnetotelluric method is a technique for imaging the electrical conductivity and structure of the Earth, from the near surface down to the 410 km transition zone and beyond. This book forms the first comprehensive overview of magnetotellurics from the salient physics and its mathematical representation, to practical implementation in the field ...
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An Interpretive Analysis of Magnetotelluric Data

Exploration Geophysics, 1984
Abstract A simple analysis to determine the dimensionality of magnetotelluric resistivity variations, to separate the near-surface resistivity variation from the variations at depth, and to find the relative resistivity variations with depth is described.
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Diagrams for magnetotelluric data

Geophysics, 1976
Abstract Observed magnetotelluric data are often transformed to the frequency domain and expressed as the relationship [E1E2]=[z11z12z21z22][H1H2] where E1, E2 and H1, H2 represent electric and magnetic components measured along two orthogonal axes (in this paper, for simplicity, to be north and east, respectively).
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The magnetotelluric inverse problem

Geophysical Surveys, 1983
The magnetotelluric inverse problem is reviewed, addressing the following mathematical questions: (a)Existence of solutions: A satisfactory theory is now available to determine whether or not a given finite collection of response data is consistent with any one-dimensional conductivity profile. (b)Uniqueness: With practical data, consisting of a finite
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Auxiliary Tools for Magnetotellurics

2020
In this chapter, we shall briefly discuss the geophysical tools that are categorised as auxiliary tools for magnetotellurics where both natural and man-made sources are used to measure both electric and magnetic fields. These tools are: (i) audiofrequency magnetotellurics (AMT), (ii) controlled-source audiofrequency magnetotellurics (CSAMT) and (iii ...
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Magnetotelluric Closed-Loop Inversion

IEEE Transactions on Geoscience and Remote Sensing, 2023
Zhuo Jia   +5 more
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