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- W1643933369 abstract "Antarctic H chondrites show a different range of induced thermoluminescence properties compared with those of H chondrites that have fallen elsewhere in the world. Recent noble gas data of Schultz et al. (1991) show that this difference is displayed most dramatically by meteorites with cosmicray exposure ages < 20 Ma, and they confirm that the differences cannot be attributed to weathering or to the presence of a great many fragments of an unusual Antarctic meteorite. Annealing experiments on an H5 chondrite, and other measurements on a variety of ordinary chondrites, have shown that induced TL properties are sensitive to the thermal histories of the meteorites. We conclude that the event(s) that released the <20 Ma samples, which are predominantly those with exposure ages of 8 ± 2 Ma, produced two groups with different thermal histories, one that came to Earth several 105 years ago and that are currently only found in Antarctica, and one that is currently falling on the Earth." @default.
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- W1643933369 date "1991-04-01" @default.
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- W1643933369 title "Evidence for differences in the thermal histories of Antarctic and non-Antarctic H chondrites with cosmic-ray exposure ages" @default.
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- W1643933369 doi "https://doi.org/10.1016/0016-7037(91)90178-8" @default.
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