Register      Login
Exploration Geophysics Exploration Geophysics Society
Journal of the Australian Society of Exploration Geophysicists
RESEARCH ARTICLE

The ratio of B-field and dB/dt time constants from time-domain electromagnetic data: a new tool for estimating size and conductivity of mineral deposits

Kun Guo 1 James E. Mungall 1 3 Richard S. Smith 2
+ Author Affiliations
- Author Affiliations

1 University of Toronto, Department of Earth Sciences, 22 Russell St, Toronto, Ontario, Canada M5S 3B1.

2 Laurentian University, Department of Earth Sciences, 935 Ramsay Lake Rd, Sudbury, Ontario, Canada P3E 2C6.

3 Corresponding author. Email: mungall@es.utoronto.ca

Exploration Geophysics 44(4) 238-244 https://doi.org/10.1071/EG13042
Submitted: 1 May 2013  Accepted: 1 August 2013   Published: 12 September 2013

Abstract

A discrete conductive sphere model in which current paths are constrained to a single planar orientation (the ‘dipping sphere’) is used to calculate the secondary response from Geotech Ltd’s VTEM airborne time domain electromagnetic (EM) system. In addition to calculating the time constants of the B-field and dB/dt responses, we focus on the time-constant ratio at a late time interval and compare numerical results with several field examples. For very strong conductors with conductivity above a critical value, both the B-field and dB/dt responses show decreasing values as the conductivity increases. Therefore response does not uniquely define conductivity. However, calculation of time constants for the decay removes the ambiguity and allows discrimination of high and low conductivity targets. A further benefit is gained by comparing the time constants of the B-field and dB/dt decays, which co-vary systematically over a wide range of target conductance. An advantage of calculating time constant ratios is that the ratios are insensitive to the dip and the depth of the targets and are stable across the conductor. Therefore we propose to use their ratio rτ = τB/τdB/dt as a tool to estimate the size and conductivity of mineral deposits. Using the VTEM base frequency, the magnitude of rτ reaches a limiting value of 1.32 for the most highly conductive targets. Interpretations become more complicated in the presence of conductive overburden, which appears to cause the limiting value of rτ to increase to 2 or more.

Key words: B-field, dB/dt, decay constant, time constant ratio, time-domain EM, overburden.


References

Abramowitz, M., and Stegun, I. A., 1965, Handbook of mathematical functions with formulas, graphs, and mathematical tables: US Government Print Off.

Asten, M. W., and Duncan, A. W., 2012, The quantitative advantage of using B-field sensors in time-domain EM measurement for mineral exploration and unexploded ordnance search: Geophysics, 77, WB137–WB148
The quantitative advantage of using B-field sensors in time-domain EM measurement for mineral exploration and unexploded ordnance search:Crossref | GoogleScholarGoogle Scholar |

Balch, S. J., Mungall, J. E., and Niemi, J., 2010, Present and future geophysical methods for Ni-Cu-PGE exploration: lessons from McFaulds Lake, Northern Ontario: SEG Special Publication 15, 559–572.

Fiset, N., Acorn, W., Legault, J., and Smith, G., 2010, Report on a helicopter-borne versatile time-domain electromagnetic (VTEM) and aeromagnetic geophysical survey: Geotech Ltd, Project 10034.

Grant, F. S., and West, G. F., 1965, Interpretation theory in applied geophysics: McGraw Hill.

Gray, M. J., 1989, 1988 Diamond Drill Programme Assessment Report - TH Option - Cartier Area: Ontario Ministry of Northern Development and Mines Assessment Report 41112NE0064 16.

Hurley, D. G., 1977, The effect of a conductive overburden on the transient electromagnetic response of a sphere: Geoexploration, 15, 77–85
The effect of a conductive overburden on the transient electromagnetic response of a sphere:Crossref | GoogleScholarGoogle Scholar |

Kuzmin, P. V., and Morrison, E. B., 2008, Bucking coil and B-field measurement and apparatus for time domain electromagnetic measurements: United States patent application publication No. US2010/0052685 A1.

Lamontagne, Y., 1975, Applications of wideband, time domain, EM measurements in mineral exploration: Ph.D. thesis, University of Toronto

McCracken, K. G., Oritaglio, M. L., and Hohmann, G. W., 1986, A comparison of electromagnetic exploration systems: Geophysics, 51, 810–818
A comparison of electromagnetic exploration systems:Crossref | GoogleScholarGoogle Scholar |

Pearce, C. I., Pattrick, R. A. D., and Vaughan, D. J., 2006, Electrical and magnetic properties of sulphides: Reviews in Mineralogy and Geochemistry, 61, 127–180
Electrical and magnetic properties of sulphides:Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BD28XosFagsbc%3D&md5=edd872c5f8d6404738bea3fc8e3697fcCAS |

Riedel, M., Willoughby E. C., and Chopra, S., 2010, Gas hydrates geophysical exploration techniques and methods, in M. Riedel, E. C. Willoughby, and S. Chopra, eds., Geophysical Characterization of Gas Hydrates: SEG Geophysical Development Series, 14, 1–22.

Smith, R. S., and Annan, A. P., 1998, The use of B-field measurement in an airborne time-domain system: Part I. Benefits of B-field versus dB/dt: Exploration Geophysics, 29, 24–29
The use of B-field measurement in an airborne time-domain system: Part I. Benefits of B-field versus dB/dt:Crossref | GoogleScholarGoogle Scholar |

Smith, R. S., and Annan, A. P., 2000, Using an induction coil sensor to indirectly measure the B-field response in the bandwidth of the transient electromagnetic method: Geophysics, 65, 1489–1494
Using an induction coil sensor to indirectly measure the B-field response in the bandwidth of the transient electromagnetic method:Crossref | GoogleScholarGoogle Scholar |

Smith, R. S., and Lee, T. J., 2001, The impulse-response moments of a conductive sphere in a uniform field, a versatile and efficient electromagnetic model: Exploration Geophysics, 32, 113–118
The impulse-response moments of a conductive sphere in a uniform field, a versatile and efficient electromagnetic model:Crossref | GoogleScholarGoogle Scholar |

Smith, R. S., and Wasylechko, R., 2012, Sensitivity cross-sections in airborne electromagnetic methods using discrete conductors: Exploration Geophysics, 43, 95–103
Sensitivity cross-sections in airborne electromagnetic methods using discrete conductors:Crossref | GoogleScholarGoogle Scholar |

Smith, R. S., and West, G. F., 1988, Inductive interaction between polarizable conductors: an explanation of a negative coincident-loop transient electromagnetic response: Geophysics, 53, 677–690
Inductive interaction between polarizable conductors: an explanation of a negative coincident-loop transient electromagnetic response:Crossref | GoogleScholarGoogle Scholar |

Ward, S. H., and Hohmann, G. W. 1988, Electromagnetic theory for geophysical applications, in M. N. Nabighian, ed., Electromagnetic methods in applied geophysics: SEG Special Volume 2, 131–311.

West, G. F., and Macnae, J. C., 1991, Physics of the electromagnetic induction exploration method, in M. N. Nabighian, ed., Electromagnetic methods in applied geophysics: SEG Special Volume 2, Part A, 1–45.