The time dependent magnetization of fine-grained iron in lunar breccias

Physics

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Scientific paper

Lunar breccias of low metamorphic grade offer a unique opportunity to investigate the magnetic properties of dispersed fine grained iron. These rocks exhibit a pronounced time dependent magnetization whose acquisition and decay are well explained by Néel's single domain theory. The effect is due to iron grains in the range of 120 Å to 150 Å in diameter which covers the transition from superparamagnetic to stable single domain behavior.

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