Abstract
The TEM method is being used increasingly for mineral exploration and geological mapping in Australia. The techniques can be divided into one-loop and coincident-loop systems (MPPO?1, MPP?3, SIROTEM) and two-loop systems (Pulse EM, Newmont EMP, SIROTEM, UTEM); the two systems exhibit markedly different responses over the conductive surface layers which cover much of Australia. Exploration in the eighties by this method will depend on developing methods of quantitative interpretation of anomalies caused by variations in the surface layer.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.