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The Leading Edge; 2005; v. 24; no. Supplement; p. S42-S45; DOI: 10.1190/1.2112391
© 2005 Society of Exploration Geophysicists
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Electrical and EM methods, 1980–2005

Misac N. Nabighian

Colorado School of Mines, Golden, USA

James C. Macnae

RMIT University, Melbourne, Australia



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Figure 1. Several half-periods of observed voltage data stacked in a SmartEM receiver, plotted as 2500 samples over a 2-s half-period. The transmitter is off for the central half of the plot. The Fluxgate (green, offset +20) and HTS (red, offset +10) data are vertically shifted from the LTS (blue) response for ease of visualization.

 


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Figure 2. (a) The two-layer case (sea and subsea). (b) The four-layer case incorporating a resistive layer situated 1000 m below the seafloor, having a thickness of 100 m and a resistivity of 100 ohm-m. The sea depth is 1 km and the transmitter frequency is 0.25 Hz.

 


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Figure 3. (a) Calculated radial electric field obtained with an inline array over the two models shown in figure 1; (b) the normalized response for variable frequencies. Sea depth is 1 km.

 





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