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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, data processing, modeling
and geological interpretation. Electromagnetic induction in 1-D,
2-D and 3-D media is explored, building from first principles, and
with thorough coverage of the practical techniques of time series
processing, distortion, numerical modeling and inversion. The
fundamental principles are illustrated with a series of case
histories describing geological applications. Technical issues,
instrumentation and field practices are described for both land and
marine surveys. This book provides a rigorous introduction to
magnetotellurics for academic researchers and advanced students,
and will be of interest to industrial practitioners and
geoscientists wanting to incorporate rock conductivity into their
interpretations.
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, data processing, modeling
and geological interpretation. Electromagnetic induction in 1-D,
2-D and 3-D media is explored, building from first principles, and
with thorough coverage of the practical techniques of time series
processing, distortion, numerical modeling and inversion. The
fundamental principles are illustrated with a series of case
histories describing geological applications. Technical issues,
instrumentation and field practices are described for both land and
marine surveys. This book provides a rigorous introduction to
magnetotellurics for academic researchers and advanced students,
and will be of interest to industrial practitioners and
geoscientists wanting to incorporate rock conductivity into their
interpretations.
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