Hi I have a question about using the analytic signal or local wavenumber for depth estimates. I see when using the local wavenumber on a magnetic grid it is often better to take a vertical integral first to reduce the noise. What I am wondering is if people usual use the RTP or TMI for generating depth estimates. I think in theory the analytic signal and local wavenumber should peak near the edges of features regardless of inclination, but I'm just wondering which grid people typically use in practice?
Any advice on using these functions would be much appreciated. Regards, Doug --- Forum archives can be accessed here: http://lyris.geosoft.com/read/?fourm=geonet You are currently subscribed to geonet as: [email protected]. To subscribe or unsubscribe from any of our forums, select the User Forum selection on the Geosoft Community page: http://www.geosoft.com/support/community
