Abstract
Geophysical measurements of electrical conductivity, magnetic fields, and gamma radiation at the Oak Ridge Reservation exhibited multifractality (fractal and multiscaling), to varying degrees, in both the north-south and east-west directions. The multiscaling was anisotropic, and the underlying statistics of the fields were in general non-Gaussian. We fitted the multifractal model of Schertzer and Lovejoy to the data. The model appears to be able to simulate a wide range of fields and to reproduce the negative skewness of the data histograms. For brevity, only our analysis of the magnetic data is reported here.
Original language | English (US) |
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State | Published - 2004 |
Externally published | Yes |
Event | 2004 Society of Exploration Geophysicists Annual Meeting, SEG 2004 - Denver, United States Duration: Oct 10 2004 → Oct 15 2004 |
Other
Other | 2004 Society of Exploration Geophysicists Annual Meeting, SEG 2004 |
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Country/Territory | United States |
City | Denver |
Period | 10/10/04 → 10/15/04 |
All Science Journal Classification (ASJC) codes
- Geophysics