Formation of the binary near‐Earth object 1996 FG3: Can binary NEOs be the source of short‐CRE meteorites?

1996 FG3 is a binary near-Earth object (NEO) that was likely formed during a tidal disruption event. Our results indicate that the formation of this binary object was unlikely to have occurred when the progenitor had a encounter velocity with the Earth significantly smaller than its current value (10.7 km/s); The formation of the binary object on an orbit similar to the present one is possible, and the survival of the satellite constrains this to have happened less than 1.6 Ma ago. However, the binary object could also have been formed when the progenitor's encounter velocity with Earth was >12 km/s, and in this case we cannot constrain its formation age. Our results indicate that tidal disruptions occurring among NEOs with low velocity encounters with Earth are unlikely to produce long-lasting NEO binaries. Thus, tidal disruption may not be able to completely re-supply the observed population. This would imply that a significant fraction of the observed NEO binaries evolved out of the main asteroid belt. Overall, our results suggest to us that the CM2 meteorites having cosmic ray exposure (CRE) ages of ~200,000 yr were likely liberated by the tidal disruption of a primitive NEO with a relative velocity with the Earth significantly smaller than that of 1996 FG3. We propose a list of such objects, although as far as we know, none of the candidates is a binary for the reasons described above.

[1]  A. Meibom,et al.  Evidence for the insignificance of ordinary chondritic material in the asteroid belt , 1999 .

[2]  M. Bailey,et al.  Vesta fragments from v6 and 3:1 resonances: Implications for V‐type near‐Earth asteroids and howardite, eucrite and diogenite meteorites , 1997 .

[3]  Michael D. Hicks,et al.  Two-Period Lightcurves of 1996 FG3, 1998 PG, and (5407) 1992 AX: One Probable and Two Possible Binary Asteroids , 2000 .

[4]  P. Spurný,et al.  The orbit and atmospheric trajectory of the Orgueil meteorite from historical records , 2006 .

[5]  M. Zolensky,et al.  Petrographic, Chemical and Spectroscopic Data on Thermally Metamorphosed Carbonaceous Chondrites , 2002 .

[6]  J. Stoer,et al.  Introduction to Numerical Analysis , 2002 .

[7]  Robert Jedicke,et al.  The fossilized size distribution of the main asteroid belt , 2003 .

[8]  John A. Wood,et al.  A chemical-petrologic classification for the chondritic meteorites. , 1967 .

[9]  Alessandro Morbidelli,et al.  The Yarkovsky-driven origin of near-Earth asteroids , 2003 .

[10]  M. Zolensky,et al.  Metamorphosed CM and CI Carbonaceous Chondrites Could be from the Breakup of the Same Earth-crossing Asteroid , 2005 .

[11]  S. Love,et al.  CAN TIDAL DISRUPTION OF ASTEROIDS MAKE CRATER CHAINS ON THE EARTH AND MOON , 1997 .

[12]  Daniel J. Scheeres,et al.  Radar Imaging of Binary Near-Earth Asteroid (66391) 1999 KW4 , 2006, Science.

[13]  Joseph A. Burns,et al.  Effects of thermal radiation on the dynamics of binary NEAs , 2004 .

[14]  D. Rubincam,et al.  Radiative Spin-up and Spin-down of Small Asteroids , 2000 .

[15]  William F. Bottke,et al.  Formation of asteroid satellites and doublet craters by planetary tidal forces , 1996, Nature.

[16]  Giovanni B. Valsecchi,et al.  Basic targeting strategies for rendezvous and flyby missions to the near-Earth asteroids , 2001 .

[17]  O. Eugster Cosmic-ray Exposure Ages of Meteorites and Lunar Rocks and Their Significance , 2003 .

[18]  D. Richardson,et al.  Binary near-Earth asteroid formation: Rubble pile model of tidal disruptions , 2005 .

[19]  Apostolos A. Christou,et al.  The statistics of flight opportunities to accessible near-Earth asteroids , 2003 .

[20]  Alessandro Morbidelli,et al.  Orbital and temporal distributions of meteorites originating in the asteroid belt , 1998 .

[21]  R. Jedicke,et al.  Debiased Orbital and Absolute Magnitude Distribution of the Near-Earth Objects , 2002 .

[22]  Giovanni B. Valsecchi,et al.  Dynamical and compositional assessment of near‐Earth object mission targets , 2004 .

[23]  D. Vokrouhlický,et al.  Yarkovsky detection opportunities. II. Binary systems , 2005 .

[24]  S. Ostro,et al.  Asteroid Radar Astronomy at the Dawn of the New Millennium , 2002 .

[25]  Stefano Mottola,et al.  Mutual Eclipse Events in Asteroidal Binary System 1996 FG3: Observations and a Numerical Model , 2000 .

[26]  W. Bottke,et al.  Origin and Evolution of Near-Earth Objects , 2002 .

[27]  T V Johnson,et al.  Asteroid Vesta: Spectral Reflectivity and Compositional Implications , 1970, Science.

[28]  D. Campbell,et al.  Binary Asteroids in the Near-Earth Object Population , 2002, Science.

[29]  Daniel D. Durda,et al.  Asteroids Do Have Satellites , 2002 .

[30]  R. Binzel,et al.  Chips off of Asteroid 4 Vesta: Evidence for the Parent Body of Basaltic Achondrite Meteorites , 1993, Science.

[31]  H. Melosh,et al.  Binary Asteroids and the Formation of Doublet Craters , 1996 .

[32]  A. Davis,et al.  Refractory inclusions from the ungrouped carbonaceous chondrites MacAlpine Hills 87300 and 88107 , 2000 .

[33]  C. F. Yoder Tidal rigidity of Phobos , 1982 .

[34]  S. Love,et al.  Tidal Distortion and Disruption of Earth-Crossing Asteroids , 1997 .

[35]  Derek C. Richardson,et al.  The formation of asteroid satellites in large impacts: Results from numerical simulations , 2004 .

[36]  S. Ostro,et al.  Radar imaging of binary near-Earth Asteroid 1998 ST 27 , 2003 .