TY - JOUR
T1 - The impact crater at the origin of the Julia family detected with VLT/SPHERE?
A1 - Vernazza, P.
A1 - Brož, M.
A1 - Drouard, A.
A1 - Hanuš, J.
A1 - Viikinkoski, M.
A1 - Marsset, M.
A1 - Jorda, L.
A1 - Fetick, R.
A1 - Carry, B.
A1 - Marchis, F.
A1 - Birlan, M.
A1 - Fusco, T.
A1 - Santana-Ros, T.
A1 - Podlewska-Gaca, E.
A1 - Jehin, E.
A1 - Ferrais, M.
A1 - Bartczak, P.
A1 - Dudziński, G.
A1 - Berthier, J.
A1 - Castillo-Rogez, J.
A1 - Cipriani, F.
A1 - Colas, F.
A1 - Dumas, C.
A1 - Ďurech, J.
A1 - Kaasalainen, M.
A1 - Kryszczynska, A.
A1 - Lamy, P.
A1 - Le Coroller, H.
A1 - Marciniak, A.
A1 - Michalowski, T.
A1 - Michel, P.
A1 - Pajuelo, M.
A1 - Tanga, P.
A1 - Vachier, F.
A1 - Vigan, A.
A1 - Warner, B.
A1 - Witasse, O.
A1 - Yang, B.
A1 - Asphaug, E.
A1 - Richardson, D. C.
A1 - Ševeček, P.
A1 - Gillon, M.
A1 - Benkhaldoun, Z.
JA - Astronomy and Astrophysics
Y1 - 2018
VL - 618
SP - A154
SN - 0004-6361
UR - https://ui.adsabs.harvard.edu/abs/2018A&A...618A.154V
KW - asteroids: individual: (89) Julia
KW - methods: numerical
KW - methods: observational
KW - minor planets
KW - techniques: high angular resolution
N2 - Context. The vast majority of the geophysical and geological constraints
M1 - ={(e.g.
M1 - internal structure
M1 - cratering history) for main-belt asteroids
M1 - have so far been obtained via dedicated interplanetary missions (e.g.
M1 - ESA Rosetta
M1 - NASA Dawn). The high angular resolution of SPHERE/ZIMPOL
M1 - the new-generation visible adaptive-optics camera at ESO VLT
M1 - implies
M1 - that these science objectives can now be investigated from the ground
M1 - for a large fraction of D ≥ 100 km main-belt asteroids. The sharp images
M1 - acquired by this instrument can be used to accurately constrain the
M1 - shape and thus volume of these bodies (hence density when combined with
M1 - mass estimates) and to characterize the distribution and topography of D
M1 - ≥ 30 km craters across their surfaces.
Aims: Here
M1 - via several
M1 - complementary approaches
M1 - we evaluated the recently proposed hypothesis
M1 - that the S-type asteroid (89) Julia is the parent body of a small
M1 - compact asteroid family that formed via a cratering collisional event.
M1 -
Methods: We observed (89) Julia with VLT/SPHERE/ZIMPOL throughout
M1 - its rotation
M1 - derived its 3D shape
M1 - and performed a reconnaissance and
M1 - characterization of the largest craters. We also performed numerical
M1 - simulations to first confirm the existence of the Julia family and to
M1 - determine its age and the size of the impact crater at its origin.
M1 - Finally
M1 - we utilized the images/3D shape in an attempt to identify the
M1 - origin location of the small collisional family.
Results: On the
M1 - one hand
M1 - our VLT/SPHERE observations reveal the presence of a large
M1 - crater (D 75 km) in Julia's southern hemisphere. On the other hand
M1 - our
M1 - numerical simulations suggest that (89) Julia was impacted 30-120 Myrs
M1 - ago by a D 8 km asteroid
M1 - thereby creating a D ≥ 60 km impact crater at
M1 - the surface of Julia. Given the small size of the impactor
M1 - the
M1 - obliquity of Julia and the particular orientation of the family in the
M1 - (a
M1 - i) space
M1 - the imaged impact crater is likely to be the origin of the
M1 - family.
Conclusions: New doors into ground-based asteroid
M1 - exploration
M1 - namely
M1 - geophysics and geology
M1 - are being opened thanks to
M1 - the unique capabilities of VLT/SPHERE. Also
M1 - the present work may
M1 - represent the beginning of a new era of asteroid-family studies. In the
M1 - fields of geophysics
M1 - geology
M1 - and asteroid family studies
M1 - the future
M1 - will only get brighter with the forthcoming arrival of 30-40 m class
M1 - telescopes like ELT
M1 - TMT
M1 - and GMT.