1993Institutional Repository National Institute of Polar Research (National Institute of Polar Research (Japan))Open access

Terrestrial ages of Antarctic meteorites measured by thermoluminescence of the fusion crust II.

Shigeyoshi Miono, A. Nakanishi

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Abstract

The acquired doses of Antarctic meteorites for dating of terrestrial ages were measured by the thermoluminescence (TL) intensity of fusion crust. It is now clearer that there is a significant correlation between the acquired dose and terrestrial age, which was previously measured by cosmogenic radionuclide abundance. Also, the ^<36>Cl method by accelerator mass spectrometry seems to provide a large terrestrial age occasionally.

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The acquired doses of Antarctic meteorites for dating of terrestrial ages were measured by the thermoluminescence (TL) intensity of fusion crust. It is now clearer that there is a significant correlation between the acquired dose and terrestrial age, which was previously measured by cosmogenic radionuclide abundance. Also, the ^<36>Cl method by accelerator mass spectrometry seems to provide a large terrestrial age occasionally.

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Available abstract

The acquired doses of Antarctic meteorites for dating of terrestrial ages were measured by the thermoluminescence (TL) intensity of fusion crust. It is now clearer that there is a significant correlation between the acquired dose and terrestrial age, which was previously measured by cosmogenic radionuclide abundance. Also, the ^<36>Cl method by accelerator mass spectrometry seems to provide a large terrestrial age occasionally.

Key concepts: Thermoluminescence, Meteorite, Crust, Fusion, Astrobiology, Geology, Earth science, Geochemistry

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