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[[terms:reduction_to_equator_seismic]]

Reduction-To-Equator (seismic)

A mathematical transformation of the total magnetic intensity field at its observed inclination (I) and declination (D) to that of the magnetic equator. I=0o.

 
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terms/reduction_to_equator_seismic.txt · Last modified: 2011/07/26 09:21 (external edit)