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This is neither an absolute age for Eros, because major impacts can potentially quot;resetquot; the asteroid surface record (27, 28), nor is it an accurate age for the current surface record, because the chaotic nature of Eros's orbit has exposed it to a highly variable impactor flux (25) rather than our assumed constant flux. At best, this surface age represents a lower limit, assuming that an average Main Belt impactor flux is at the high end of those to which Eros has actually been exposed.
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We thank H. Kanamori (California Institute of Technology) for the use of his theoretical seismic code for Lamb pulse seismic sources, C. Chapman (Southwest Research Institute) for the use of his crater count data for Eros, and D. O'Brien (University of Arizona) for the use of his modeling results for the collisional history of the main asteroid belt. Supported by grant no. NAG5-12619 of NASA's NEAR Data Analysis Program and no. NAG5-11493 of NASA's Planetary Geology and Geophysics Program.
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