The age of the meteorite recovery surfaces of Roosevelt County, New Mexico, USA

• Published in: Meteoritics
• Main Authors: Zolensky, Michael E., Rendell, Helen M., Wilson, Ivan, Wells, Gordon L.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1992
• Subjects: Antarc*; Antarctica
• Online Access: http://dx.doi.org/10.1111/j.1945-5100.1992.tb00228.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1945-5100.1992.tb00228.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1945-5100.1992.tb00228.x

Abstract— We have obtained minimum age estimates for the sand units underlying the two largest meteorite deflation surfaces in Roosevelt County, New Mexico, USA, using thermoluminescence dating techniques. The dates obtained ranged from 53.5 (±5.4) to 95.2 (±9.5) ka, and must be considered lower limits for the terrestrial ages of the meteorites found within these specific deflation surfaces. These ages greatly exceed previous measurements from adjacent meteorite‐producing deflation basins. We find that Roosevelt County meteorites are probably terrestrial contemporaries of the meteorites found at most accumulation zones in Antarctica. The apparent high meteorite accumulation rate reported for Roosevelt County by Zolensky et al . (1990) is incorrect, as it used an age of 16 ka for all Roosevelt County recovery surfaces. We conclude that the extreme variability of terrestrial ages of the Roosevelt County deflation surfaces effectively precludes their use for calculations of the meteorite accumulation rate at the Earth's surface.