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We have presented a scheme to invert satellite magnetic data for a global depth profile of mantle conductivity.
We have presented a 3-D frequency domain inversion scheme to invert satellite magnetic data for global mantle conductivity.
We have inverted the midlatitude magnetic data for this event with the results as shown in Fig. 3.
The available magnetic data for this study have been corrected for the diurnal variations, instrument drift, and for the errors in positioning and height keeping.
Magnetic data for both the complexes 1 and 2 have been fitted using the Fisher formula for S = 2 system and show antiferromagnetic coupling for both the complexes.
We applied the methods of Spector and Grant ([1970]), Okubo et al. ([1985]) and Trifonova et al. ([2006]), which examined the spectral knowledge included in subregions of magnetic data for our analysis.
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GEOMAGIA50.v3 for sediments builds upon the structure of the pre-existing GEOMAGIA50 database for magnetic data from archeological and volcanic materials.
We thank USGS for validating the scalar magnetometer, and for providing magnetic data from the Honolulu observatory.
Maus et al. (2007) obtained a value of 15 km as the correlation length for gridded magnetic data of the former Soviet Union, Australia, and North America.
In such cases, we referred to the magnetic data from the nightside station (TAM for dawn side events and TUC for dusk side events) and removed any events that had no clear Pi2 signature in the nightside data.
These advantages hold true for practical field magnetic data from the Hawsons mining area in Australia, verifying the effectiveness of the proposed scheme.
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