Transcript Designing Borehole IP Surveys
Designing Borehole IP Surveys
By Joe Mihelcic, Geophysicist ClearView Geophysics Inc.
Ontario Exploration & Geoscience Symposium “New Ideas, Revisiting Past Discoveries” December 7, 2010
What is Borehole IP (BHIP)?
Any induced polarization survey that utilizes boreholes to: Inject current or Measure potentials
When is BHIP applied?
Most common scenario is that favourable mineralization intersected in at least one borehole: Test if target is chargeable Quantify in or around borehole Determine Orientation/Direction/Extents Prioritize available geophysics and drilling data
How to achieve this with BHIP?
Many configurations and methods available: Mise-a-la-masse In-hole Pole-dipole and dipole-dipole Hole-to-hole Gradient Etc. etc.
Designing BHIP surveys
Keep it simple Configure using basic physics Include external data Consider cost/risk vs. benefit/reward E.g., tomographic mode for mineral exploration?
Example:
Favourable mineralization detected in a number of boreholes spread over wide area Favoured theory suggests overall mineralizatoin plunges towards the northwest Attempt BHIP to test this theory from borehole with good intersection 158.2 m -193.6 m
Step 1
Run a simple dipole-dipole detection log to determine if intersected zone is chargeable:
Step 2
Charge the target zone with Current Electrodes above and below the zone: C1 = 162 m (VG at 176 m) C2 = 225 m Read potentials on surface Ensure lines at 90 degrees to BH direction Tie-in to surface BH’s (bush crash)
Step 2
Axis ‘A’ identified along chargeability trend
Step 2
Axis ‘A’ identified along chargeability trend
Step 3
Compare to available geophysics data
Step 3
Compare to available geophysics data
Step 3
Compare to available geophysics data
Step 4:
Focused post-processing of previously acquired surface pole-dipole geophysics data Inversion modeling Overlay drilling locations in 3D
Step 4:
- Not available on website download due to size - Available upon request
Step 5:
Which boreholes drilled through zone?
Re-examine logs to find anomaly source Recommend tighter drilling along source axis if favourable intersections already encountered
Conclusions:
BHIP requires more customization than standard surface arrays Inversion modeling useful in some cases, at end of process, especially for 3D visualization A method to further prioritize surface IP results