Physics
Scientific paper
Jan 1996
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996m%26ps...31...77t&link_type=abstract
Meteoritics and Planetary Science, Vol. 31, p. 77-80 (1996)
Physics
Scientific paper
We extracted black, magnetic spherules from well cuttings of Oligocene sediments in the coastal plain of South Carolina, USA. Three possible origins were considered: industrial, volcanic, and extra- terrestrial. An extraterrestrial origin by ablation of parent meteoroid material is proposed, based on the spherule morphologies, the presence of metallic Fe cores in many of the spherules, and the detection of wüstite in some of the oxide rims. Low Ni contents are problematic but may be attributed to the ablation of a low-Ni parental body, such as hexahedrite. The presence of spherules in somewhat clay-like, sandy sediments is unusual, as most magnetic spherules are found in abyssal muds. Based on benthic foraminiferal assemblages and sediment distribution above, within, and below the beds containing spherules, it is unlikely that the spherules were transported from a deep-sea environment.
Fronabarger A. K.
Katuna M. P.
Nusbaum R. L.
Summer N.
Taylor Peter L.
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