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pro vyhledávání: '"John M Stanley"'
Autor:
John M Stanley, Phillip W Schmidt
Publikováno v:
Preview. 2020:8-10
The development of optically pumped magnetometer systems and their applications in Australia: Part 2
Autor:
John M. Stanley
Publikováno v:
Preview. 2017:42-49
Autor:
John M. Stanley
Publikováno v:
Preview. 2016:46-53
Autor:
Lisa Worrall, David Annetts, Leslie Atkinson, Phil Harman, Roger Henderson, Todd Mojesky, Marina Costelloe, Mark Lackie, Stephanie Kovach, Ron Palmer, Kate Robertson, Mark Duffett, Thong Huynh, John M Stanley, Phillip W Schmidt, John Denham, Ken Witherly, Mike Barlow, Ned Stolz, Stephan Thiel, David Howard, David Denham, Mike Hatch, Terry Harvey, Michael Micenko, Tim Keeping, Ian James, Rod Paterson, Michael Asten, E. T. Eadie, J. Silic, D. J. Jack
Publikováno v:
Preview. 2020:i-i
Publikováno v:
Exploration Geophysics. 36:198-205
Sub-Audio Magnetics (SAM) is a method by which a total-field magnetic sensor may be used to simultaneously acquire both total magnetic intensity (TMI) and total-field electromagnetic induction (TFEMI) responses from buried metal. In situations where
Publikováno v:
Exploration Geophysics. 24:387-399
A high definition technique has been developed for simultaneously mapping electrical and magnetic characteristics of the ground. Each of the parameters may be measured at sub-metre intervals while ...
Publikováno v:
Exploration Geophysics. 23:323-326
Exploration beneath a near-surface white magnetic noise source, such as maghemitic and lateritic soils or thin basalt flows, can best be achieved at ground level. The objective of such exploration is to discriminate between the noise and signal from
Autor:
John M. Stanley, Malcolm K. Cattach
Publikováno v:
Exploration Geophysics. 21:91-103
Recent advances in magnetometer technology have resulted in high-definition magnetic mapping becoming a rapid and effective aid to engineering site investigation. Conventional magnetometer systems were usually too slow to be economical for mapping ma
Autor:
John M, Stanley
Publikováno v:
The Hastings Center report.
Autor:
John M. Stanley, J. Zhou
Publikováno v:
Exploration Geophysics. 24:879-881
The interpretation of a magnetic anomaly profile is achieved by solving a Fredholm integral equation of the first kind. Numerical solutions to such a problem require the conversion from the original form to a system of linear equations. The commonly