The discovery and significance of a fossilized radiogenic argon wave (argonami) in the earth's crust

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Argon Isotopes, Biotite, Earth Crust, Radioactive Isotopes, Grain Size, Tectonics

Scientific paper

The discovery of a 'fossilized' asymmetric radiogenic argon wave (argonami) trapped in single grains of biotite in the contact zones between a diabase dike and the Grenville country rock near Mattawa, Ontario, Canada, is reported. The phenomenon is argued to be the result of the interplay between the partial pressure of the ambient radiogenic argon and the opening and closing (blocking) of biotite to argon movement during the period of thermal and perturbation following the dike intrusion. The occurrence of the argonami phenomenon suggests that, in some instances, the analysis of excess argon may become a useful tool for elucidating complex tectonothermal and fluid-migratory events taking place at plate boundaries and igneous contacts.

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