Terrestrial ages of Antarctic meteorites measured by thermoluminescence of the fusion crust II.
Shigeyoshi Miono, A. Nakanishi
Abstract
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Shigeyoshi Miono, A. Nakanishi
Abstract
Open-access reader
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.
Key concepts: Thermoluminescence, Meteorite, Crust, Fusion, Astrobiology, Geology, Earth science, Geochemistry