Deep Electromagnetic Sounding
Deep Electromagnetic Sounding is a geophysical method that employs low-frequency electromagnetic fields to probe and characterize the electrical conductivity structure of the Earth's subsurface at depths typically exceeding several kilometers, distinguishing it from shallower electromagnetic surveying techniques by its focus on regional to lithospheric-scale investigations.
88
Publications
3.5K
Citations
247
Authors
123
Institutions
Publications per year
2017–2026
9
Variants
Deep Electromagnetic Soundings
Parents
88
Controlled-source electromagnetic sounding of the oceanic lithosphere
Charles S. Cox, Steven Constable, Alan D. Chave et al. · Nature · 1986 · 212 citations
1–5 of 88
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Institute of Geophysics Polish Academy of Sciences, Poland
3 publications · 38 citations
3
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1–5 of 247
123

University of Cologne
Cologne, Germany
7 h-index
16 publications
566 citations
Institute of Terrestrial Magnetism Ionosphere and Radio Wave Propagation
Moscow, Russia
6 h-index
16 publications
313 citations
National Geophysical Research Institute
Hyderabad, India
5 h-index
6 publications
122 citations
University of California, Berkeley
Berkeley, United States
4 h-index
4 publications
91 citations

Scripps Institution of Oceanography
La Jolla, United States
4 h-index
8 publications
940 citations
Federal Institute for Geosciences and Natural Resources
Hanover, Germany
3 h-index
8 publications
386 citations
Institute of Geophysics Polish Academy of Sciences
Warsaw, Poland
3 h-index
4 publications
53 citations
Geological Survey of Canada
Ottawa, Canada
3 h-index
3 publications
69 citations
1–8 of 123
13 publications · 632 citations
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GJI · 11 publications · 632 citations
11
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6 publications · 205 citations
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4 publications · 302 citations
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3 publications · 90 citations
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