Nickel-iron spherules in tektites: non-meteoritic in origin |
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Authors: | R Ganapathy John W Larimer |
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Institution: | 1. Research Laboratory, J.T. Baker Chemical Company, Phillipsburg, NJ 08865 U.S.A.;2. Department of Geology, Arizona State University, Tempe, AZ 85287 U.S.A. |
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Abstract: | The concentrations of several diagnostic trace elements were determined in two comparatively large NiFe spherules extracted from tektites. The purpose of the study was to obtain some clues about the chemistry of the projectile that is presumed responsible for the formation of these tektites. However, the trace element pattern is distinctly terrestrial implying that the spherules are the result of in-situ reduction of the host rock and are not meteoritic in origin. |
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