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Königsberger ratio

Königsberger ratio (Q, Qn) Originally the ratio (Q) of the intensity of natural remanent magnetization (NRM) of an igneous rock to the intensity of magnetization induced at room temperature in a magnetic field the same as that in which the original NRM was acquired. Now it usually means the ratio (Qn) of the intensity of NRM to that induced in a magnetic field of 50μT at room temperature.

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