TY - JOUR
T1 - The shape of (7) Iris as evidence of an ancient large impact?
A1 - Hanuš, J.
A1 - Marsset, M.
A1 - Vernazza, P.
A1 - Viikinkoski, M.
A1 - Drouard, A.
A1 - Brož, M.
A1 - Carry, B.
A1 - Fetick, R.
A1 - Marchis, F.
A1 - Jorda, L.
A1 - Fusco, T.
A1 - Birlan, M.
A1 - Santana-Ros, T.
A1 - Podlewska-Gaca, E.
A1 - Jehin, E.
A1 - Ferrais, M.
A1 - Grice, J.
A1 - Bartczak, P.
A1 - Berthier, J.
A1 - Castillo-Rogez, J.
A1 - Cipriani, F.
A1 - Colas, F.
A1 - Dudziński, G.
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 - Witasse, O.
A1 - Yang, B.
JA - Astronomy and Astrophysics
Y1 - 2019
VL - 624
SP - A121
SN - 0004-6361
UR - https://ui.adsabs.harvard.edu/abs/2019A&A...624A.121H
KW - asteroids: individual: 7 Iris
KW - Astrophysics - Earth and Planetary Astrophysics
KW - methods: numerical
KW - methods: observational
KW - minor planets
N2 - Context. Asteroid (7) Iris is an ideal target for disk-resolved imaging
M1 - ={owing to its brightness (V 7-8) and large angular size of 0.33'' during
M1 - its apparitions. Iris is believed to belong to the category of large
M1 - unfragmented asteroids that avoided internal differentiation
M1 - implying
M1 - that its current shape and topography may record the first few 100 Myr
M1 - of the solar system's collisional evolution.
Aims: We recovered
M1 - information about the shape and surface topography of Iris from disk-
M1 - resolved VLT/SPHERE/ZIMPOL images acquired in the frame of our ESO large
M1 - program.
Methods: We used the All-Data Asteroid Modeling (ADAM)
M1 - shape reconstruction algorithm to model the 3D shape of Iris
M1 - using
M1 - optical disk-integrated data and disk-resolved images from SPHERE and
M1 - earlier AO systems as inputs. We analyzed the SPHERE images and our
M1 - model to infer the asteroid's global shape and the morphology of its
M1 - main craters.
Results: We present the 3D shape
M1 - volume-equivalent
M1 - diameter Deq = 214 ± 5 km
M1 - and bulk density ρ = 2.7 ± 0.3 g
M1 - cm-3 of Iris. Its shape appears to be consistent with that of
M1 - an oblate spheroid with a large equatorial excavation. We identified
M1 - eight putative surface features 20-40 km in diameter detected at several
M1 - epochs
M1 - which we interpret as impact craters
M1 - and several additional
M1 - crater candidates. Craters on Iris have depth-to-diameter ratios that
M1 - are similar to those of analogous 10 km craters on Vesta.
M1 - Conclusions: The bulk density of Iris is consistent with that of its
M1 - meteoritic analog based on spectroscopic observations
M1 - namely LL
M1 - ordinary chondrites. Considering the absence of a collisional family
M1 - related to Iris and the number of large craters on its surface
M1 - we
M1 - suggest that its equatorial depression may be the remnant of an ancient
M1 - (at least 3 Gyr) impact. Iris's shape further opens the possibility that
M1 - large planetesimals formed as almost perfect oblate spheroids. Finally
M1 - we attribute the difference in crater morphology between Iris and Vesta
M1 - to their different surface gravities
M1 - and the absence of a substantial
M1 - impact-induced regolith on Iris.