Two-dimensional interpretation of three-dimensional magnetotelluric data: an example of limitations and resolution
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/150/1/127/1593287/150-1-127.pdf
Reference40 articles.
1. Bahr, K. , 1991. Geological noise in magnetotelluric data: A classification of distortion types, Phys. Earth planet. Inter., 66, 24-38.
2. Bailey, R.C. & Groom, R.W. , 1987. Decomposition of the magnetotelluric impedance tensor which is useful in the presence of channeling, Exp. Abstr. 57th ann. Inter. S. exp. geophys., Tulsa, 57, 154-156.
3. Chakridi, R. , Chouteau, M. & Mareschal, M. , 1992. A simple technique for analysing and partly removing galvanic distortion from the magnetotelluric impedance tensor: Application to Abitibi and Kapuskasing data (Canada), Geophys. J. Int., 108, 917-929.
4. 2-D Inversion of 3-D magnetotelluric data: the Kayabe dataset;García;Earth, Planets and Space,1999
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