1887
ASEG2009 - 20th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Introduction

The HeliGEOTEM system was introduced in 2005 to provide greater operational flexibility and improved lateral resolution compared with a fixed-wing system (Fountain et al., 2005). The system, described in more detail by Fountain et al. (2005), is a vertical-axis dipole transmitter towed below and behind a helicopter. The receiver, also attached to the tow cable is about 15 m in front and 35 m above the transmitter. The system measures the response in the time domain when a half-sine current pulse excites the ground. The dB/dt and B-field responses are measured in the x, y and z orientations. The geometry of the system and the coordinate system are shown on Figure 1. Compared with fixed-wing systems, the helicopter systems have their transmitter / receiver closer to the ground surface, which is why the spatial resolution is greater (the response is much sharper); also, the response of shallow bodies is much larger. However, when the bodies are deeper, the responses are more comparable.

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/content/journals/10.1071/ASEG2009ab065
2009-12-01
2026-01-15
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References

  1. Balch, S.J., Boyko, W.P. and Patersen, N.R., 2003, The AeroTEM airborne electromagnetic system: The Leading Edge 22, 562-566.
  2. Fountain, D., Smith, R., Payne, T., Lemieux, J., 2005, The HeliGEOTEM helicopter time-domain EM system applied to mineral exploration: system and data: First Break 23, November, 73-78.
  3. Macnae, J., 2008, Comparing airborne electromagnetic systems: Preview, April, 24-29.
  4. Smith R.S., Edwards R.N. and Buselli G. 1994. An automatic technique for presentation of coincident-loop, impulse-response, transient, electromagnetic data. Geophysics 59, 1542-1550.
  5. Wolfgram P. and Karlik G. 1995. Conductivity-depth transform of GEOTEM data. Exploration Geophysics 26, 179-185.
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