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| | -Sesimic Refraction
| | -Seismic Reflection
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| | -EM- Mapping Geology
| | -EM- Metal Detection
| | -Gravity
| | -Cross-Hole
| | -S-Wave Refraction
| | -Surface Wave Analysis
| | -Self Potential
| | -Magnetics
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| | -Borehole Methods
| | -Thermal Gradients
| | -Induced Polarization
| | -Seismic Monitoring
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Borehole Methods (M-14)

  1. Q: How does it work?
    A:
    A variety of tools and measurements can be made in a borehole. Acoustic, electrical, radiometric, gravitational and magnetic measurements can be made. There are over 50 types of logs offered commercially and probably ten times that many have been tried.

  2. Q: What is the geologic model?
    A: Almost any property of earth materials can be estimated by use of borehole methods. The proper method is linked to the geologic problem to be solved.

  3. Q: What are the requirements?
    A: A borehole or several boreholes completed to the specifications for the technique to be used.

  4. Q: What are the pitfalls?
    A: Borehole preparation, borehole caliper, calibration of tools, and trained operators are among the fine points of execution to be considered for a successful borehole campaign. Results are valid at the borehole and interpretation is required to interpolate between boreholes.

  5. Q: What logistics are needed?
    A: Crew size is one person with logging truck and tools. Some portable instruments and winches are available but a rig has to reach the site so driving to the site is usually no problem.

  6. Q: What are the deliverables?
    A: Deliverables are profiles of the tool response vs. depth along with maps and a narrative discussion of the work performed.

  7. Website under construction: (There is no additional information about borehole methods available at this time. Please come back later.)