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* - orbital type derived from osculating orbital elements
# - absolute magnitude H derived from astrometric observation via orbit determination - G value assumed to be 0.15
! - quality code according to Lagerkvist et al. (1989)
( 1) M.P.E.C. 2000-E14
( 2) Binzel, R.P. et al. (2004) Icarus 170, 259-294. (Observed spectral properties of near-Earth objects: results for population distribution, source regions, and space weathering processes.)
( 3) Binzel, R.P. et al. (2002) in "Asteroids III" (Eds. W.F.Bottke et al.), Univ.Ariz.Press, Tucson, USA, pp. 255-271. (Physical Properties of NEOs)
( 4) Binzel, R.P. et al. (2002) in "Asteroids III" (Eds. W.F.Bottke et al.), Univ.Ariz.Press, Tucson, USA, pp. 255-271. (Physical Properties of NEOs)
( 5) Whiteley, R.J. et al. (2002) Proceedings of ACM2002, ESA-SP500, pp. 473-480. (Monolithic fast-rotating asteroids) (H-values and rotation properties of 36 NEAs)
( 6) Whiteley, R.J. et al. (2000) B.A.A.S. 32, 1003. (Lightcurve analysis of 4 monolithic fast-rotating asteroids.) (2000 AG6, 2000 DO8, 2000 EB14, 2000 HB24)
( 7) Whiteley, R.J. et al. (2002) Icarus 157, 139-154. (Lightcurve Analysis of Four New Monolithic Fast-Rotating Asteroids) (2000 AG6,2000 DO8, 2000 EB14,2000 HB24)
( 8) Whiteley, R.J. et al. (2002) Proceedings of ACM2002, ESA-SP500, pp. 473-480. (Monolithic fast-rotating asteroids) (H-values and rotation properties of 36 NEAs)
( 9) Binzel, R.P. et al. (2004) Icarus 170, 259-294. (Observed spectral properties of near-Earth objects: results for population distribution, source regions, and space weathering processes.)
NEODyS Page of 2000 DO8