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Russell and co-workers [S. S. Russell, G. Srinivasan, G. R. Huss, G. J. Wasserburg, G. J. MacPherson, Science 273, 757 (1996); S. S. Russell, G. R. Huss, G. J. MacPherson, G. J. Wasserburg, Lunar Planet. Sci. XXVIII, 1209 (1997)] found three Chondrules with Mg isotopic anomalies, but at a lower level than in CAIs, in the meteorites Chainpur, Inman, and Semarkona, implying they formed 1 to 2 million years after CAIs. Other Chondrules in the same meteorites lack detectable Mg anomalies and apparently formed at least 1 to 3 million years later. Magnesiumchromium and iodine-xenon dating also indicate formation over an interval of several million years [T. Swindle et al., in (1), p. 77].
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T. Swindle et al., in (1), p. 77
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Russell and co-workers [S. S. Russell, G. Srinivasan, G. R. Huss, G. J. Wasserburg, G. J. MacPherson, Science 273, 757 (1996); S. S. Russell, G. R. Huss, G. J. MacPherson, G. J. Wasserburg, Lunar Planet. Sci. XXVIII, 1209 (1997)] found three Chondrules with Mg isotopic anomalies, but at a lower level than in CAIs, in the meteorites Chainpur, Inman, and Semarkona, implying they formed 1 to 2 million years after CAIs. Other Chondrules in the same meteorites lack detectable Mg anomalies and apparently formed at least 1 to 3 million years later. Magnesiumchromium and iodine-xenon dating also indicate formation over an interval of several million years [T. Swindle et al., in (1), p. 77].
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A radial pressure gradient causes the gaseous component of the nebula to rotate at slightly less than the Keplerian orbital velocity. Solid objects are subjected to gas drag, causing them to lose angular momentum and move inward [I. Adachi, C. Hayashi, K. Nakazawa, Prog. Theor. Phys. 56, 1756 (1976); S. J. Weidenschilling, Mon. Not. R. Astron. Soc. 180, 57 (1977)].
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A radial pressure gradient causes the gaseous component of the nebula to rotate at slightly less than the Keplerian orbital velocity. Solid objects are subjected to gas drag, causing them to lose angular momentum and move inward [I. Adachi, C. Hayashi, K. Nakazawa, Prog. Theor. Phys. 56, 1756 (1976); S. J. Weidenschilling, Mon. Not. R. Astron. Soc. 180, 57 (1977)].
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6844238449
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note
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-3 cm) grains are accelerated quickly because of their large area:mass ratio and experience little heating. Bodies larger than approximately centimeter size are heated too slowly to be melted by transient shocks.
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6844263735
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note
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For small eccentricity, orbital decay is primarily due to the non-Keplerian rotation of the nebula. If the eccentricity is large compared with the fractional deviation from the Kepler velocity, there is an additional secular decay of the semimajor axis as well as damping of inclination; see Adachi et al. (77).
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39
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6844233365
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note
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Our cases were computed in three dimensions, with initial inclinations between 0° and 1°. There was no significant increase in mean inclination during evolution in resonance.
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41
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0006334018
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p are the mean longitudes of Jupiter and the planetesimal, and ω + ̃is the plane-tesimal's longitude of perihelion; see F. Marzari, H. Scholl, L. Tomasella, and V. Vanzani [Planet. Space , Sci. 45, 337 (1997)].
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Scholl, H.2
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42
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R. Binzel, T. Gehrels, M. Matthews, Eds. Univ. of Arizona Press, Tucson
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Beyond 3.5 AU, the asteroid belt is dominated by low-albedo objects believed to consist of primitive, organic-rich material. Some examples of these types are found in the inner belt [J. C. Gradie, C. R. Chapman, E. F. Tedesco, in Asteroids II, R. Binzel, T. Gehrels, M. Matthews, Eds. (Univ. of Arizona Press, Tucson, 1989), p. 316].
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Tedesco, E.F.3
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44
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6844235453
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note
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We thank T. Swindle, T. V. Ruzmaikina, and J. A. Wood for discussions. Supported by NASA (S.J.W. and L.L.H.) and the Italian Space Agency (P.M.). This is Planetary Science Institute Contribution 343.
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