Dating Jilin and constraints on its temperature history

Computer Science

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Chondrites, Meteoritic Composition, Radioactive Age Determination, Temperature Distribution, Argon Isotopes, Helium Isotopes, Outgassing, Meteorites, Jilin, H5 Chondrites, Stone Meteorites, Samples, Meteorite, Dating Techniques, Ages, Argon, Release Patterns, Diffusion, Models, Parameters, Outgassing, Helium, Isotopes, Thermal History, Heating, Calculations, Temperature, Parent Bodies, Experiments, Procedure

Scientific paper

Two samples from the main mass, and one from a field fragment, of the Jilin (H5) meteorite have been dated by the Ar-40 Ar-39 technique. He-4 and Ar release patterns from a nonirradiated sample were also determined, in order to obtain diffusion parameters. Concordant Ar-40 - Ar-39 ages of about 4.0 AE indicate that Jilin was totally degassed at that time. Model calculations suggest that the heating event, 400,000 years ago, was mode-rate and brief and occurred at the separation from the parent body. Such heating at separation could be a common phenomenon, explaining late disturbances in some isotope systems.

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