Using C-14 and C-14 - Be-10 for Terrestrial Ages of Desert Meteorites

Details Using C-14 and C-14 - Be-10 for Terrestrial Ages of Desert Meteorites Using C-14 and C-14 - Be-10 for Terrestrial Ages of Desert Meteorites

Jan 2000

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000lpico.997...41j&link_type=abstract

Workshop on Extraterrestrial Materials from Cold and Hot Deserts, p. 41

Physics

Arid Lands, Meteorites, Carbon 14, Beryllium Isotopes, Antarctic Regions, Collection, Deserts, Position (Location)

Scientific paper

The arid regions of the world appear to be great storage locations for meteorites, where they can survive for long periods of time in such environments. Large numbers of meteorites have been recovered from diverse areas of and and semi-arid regions of North Africa, Arabia, North America and Western Australia. The cold desert of Antarctica is a further storehouse of meteorites. One of the first recognized areas for collections of meteorites was Roosevelt County, New Mexico. The Nullarbor region of Australia and the northern Sahara Desert in Africa are also prolific sources of meteorites.

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