Dictionary:Koenigsberger ratio (Q)

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{{#category_index:K|Koenigsberger ratio (Q)}} (kā’ nigs ber, g∂r) The ratio of the remanent magnetization to the induced magnetization (product of susceptibility and the Earth’s magnetic field strength). A large Q indicates that the magnetic material will tend to maintain significant remanent magnetization and indicates small mineral grain size. See Hood (1964).