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GEOPHYSICAL STUDIES SITE B

GEOPHYSICAL STUDIES SITE B. GEOPHYSICAL STUDIES PROGRESS OSPER PROJECT SITE B. BRUCE SMITH ROBERT BISDORF RAY HUTTON MARK TABACHECK ROBERT HORTON. GEOPHYSICAL METHODS USED. DC RESISTIVITY SOUNDING obtain variation in electrical resistivity as a function

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GEOPHYSICAL STUDIES SITE B

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  1. GEOPHYSICAL STUDIES SITE B GEOPHYSICAL STUDIES PROGRESS OSPER PROJECT SITE B BRUCE SMITH ROBERT BISDORF RAY HUTTON MARK TABACHECK ROBERT HORTON

  2. GEOPHYSICAL METHODS USED • DC RESISTIVITY SOUNDING • obtain variation in electrical resistivity as a function • of depth (to about 40 meters) • ELECTROMAGNETIC PROFILING (EM31) • obtain variation in electrical conductivity as a function • of position (mapping lateral variations) 3 to 6 meters • TOTAL FIELD MAGNETICS (not discussed) geologic mapping detect magnetic metallic objects (oil field pipes etc.) • ELECTROMAGNETIC PROFILE (EM34…not discussed) • depth to 40m but very noisy due to metallic pipes

  3. DC RESISTIVITY

  4. B SITE LOCATIONDC RESISTIVITY SOUNDINGS

  5. DC SOUNDINGS SITE B

  6. ELECTRICAL CROSS SECTION SITE B RESISTIVITY (ohm meters) CONDUCTIVITY (millisiemens) ρ = 1000/σ(ms) σ(ms) = 1000/ρ 100 ohm meters = 10 ms

  7. WEATHERED BEDROCK RESISTIVITY SOUNDING SITE B CONDUCTIVITY 1000 100 10

  8. EM31 CONDUCTIVITY SURVEY Vertical dipoles depth ~4.5m Horizontal dipoles depth ~2.25m

  9. EM31 HMD 2.25m depth map

  10. EM31 VMD 4m depth map

  11. EM31 HMD 4m 1960 Photo

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