Terrestrial ages of Antarctic meteorites: Implications for concentration mechanisms
Antarctic meteorites differ from meteorites fallen in other places in their mean terrestrial ages. Boeckl estimated the terrestrial half-life for the disintegration of stone meteorites by weathering under the climatic conditions of the Western United States to be about 3600 years. Antarctic meteorit...
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Format: | Other/Unknown Material |
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1986
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Online Access: | http://hdl.handle.net/2060/19860019355 |