Hydrocode simulations of the largest crater on asteroid Lutetia

The flyby of the Main Belt asteroid Lutetia by the Rosetta spacecraft allows the camera OSIRIS to obtain very good images of about half of the body at the maximum resolution of 60 m per pixel. From the images and radio-science experiment, a density of about (3.4±0.3) g/cm3 has been inferred for the...

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Published in:Planetary and Space Science
Main Authors: Cremonese, G., Martellato, E., Marzari, F., Kührt, E., Scholten, F., Preusker, Frank, Wünnemann, K., Borin, P., Massironi, M., Simoni, E., Ip, W-H., OSIRIS, team
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 2012
Subjects:
Online Access:https://elib.dlr.de/78590/
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author Cremonese, G.
Martellato, E.
Marzari, F.
Kührt, E.
Scholten, F.
Preusker, Frank
Wünnemann, K.
Borin, P.
Massironi, M.
Simoni, E.
Ip, W-H.
OSIRIS, team
author_facet Cremonese, G.
Martellato, E.
Marzari, F.
Kührt, E.
Scholten, F.
Preusker, Frank
Wünnemann, K.
Borin, P.
Massironi, M.
Simoni, E.
Ip, W-H.
OSIRIS, team
author_sort Cremonese, G.
collection Unknown
container_issue 1
container_start_page 147
container_title Planetary and Space Science
container_volume 66
description The flyby of the Main Belt asteroid Lutetia by the Rosetta spacecraft allows the camera OSIRIS to obtain very good images of about half of the body at the maximum resolution of 60 m per pixel. From the images and radio-science experiment, a density of about (3.4±0.3) g/cm3 has been inferred for the asteroid. Many impact craters have been observed on the surface of Lutetia and the largest, named Massilia, has a diameter of about 55 km. Relative to the size of Lutetia (the longest axis is approximately 126 km) the crater represents one of the dominating features on its surface. Whether or not the impact that formed Massilia affected the entire asteroid can be only evaluated via numerical modeling, with hydrocodes, of the impact process. The results of a suite of iSALE simulations are compared with the crater profile derived from the Digital Terrain Model of the observed surface. The best match to the DTM of the crater with hydrocode simulations has allowed to determine a value of 7.5 km for the impactor diameter, which suggests a primordial origin of Lutetia due to the low probability of such an impact event. A second interesting impact structure has been identified nearby Massilia within the North Pole Crater Cluster. The crater has a diameter of 24 km and it lies over a larger crater of the North Pole Crater Cluster. This is strongly suggestive of a very young structure on Lutetia. The numerical simulations of this feature constrain the impactor to be 3.8 km in diameter, assuming the same material properties for target and impactor as in the model of the formation of Massilia.
format Article in Journal/Newspaper
genre North Pole
genre_facet North Pole
geographic North Pole
geographic_facet North Pole
id ftdlr:oai:elib.dlr.de:78590
institution Open Polar
language unknown
op_collection_id ftdlr
op_container_end_page 154
op_doi https://doi.org/10.1016/j.pss.2012.01.001
op_relation Cremonese, G. und Martellato, E. und Marzari, F. und Kührt, E. und Scholten, F. und Preusker, Frank und Wünnemann, K. und Borin, P. und Massironi, M. und Simoni, E. und Ip, W-H. und OSIRIS, team (2012) Hydrocode simulations of the largest crater on asteroid Lutetia. Planetary and Space Science, 66 (1), Seiten 147-154. Elsevier. doi:10.1016/j.pss.2012.01.001 <https://doi.org/10.1016/j.pss.2012.01.001>.
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spelling ftdlr:oai:elib.dlr.de:78590 2025-06-15T14:43:53+00:00 Hydrocode simulations of the largest crater on asteroid Lutetia Cremonese, G. Martellato, E. Marzari, F. Kührt, E. Scholten, F. Preusker, Frank Wünnemann, K. Borin, P. Massironi, M. Simoni, E. Ip, W-H. OSIRIS, team 2012 https://elib.dlr.de/78590/ unknown Elsevier Cremonese, G. und Martellato, E. und Marzari, F. und Kührt, E. und Scholten, F. und Preusker, Frank und Wünnemann, K. und Borin, P. und Massironi, M. und Simoni, E. und Ip, W-H. und OSIRIS, team (2012) Hydrocode simulations of the largest crater on asteroid Lutetia. Planetary and Space Science, 66 (1), Seiten 147-154. Elsevier. doi:10.1016/j.pss.2012.01.001 <https://doi.org/10.1016/j.pss.2012.01.001>. Asteroiden und Kometen Zeitschriftenbeitrag PeerReviewed 2012 ftdlr https://doi.org/10.1016/j.pss.2012.01.001 2025-06-04T04:58:07Z The flyby of the Main Belt asteroid Lutetia by the Rosetta spacecraft allows the camera OSIRIS to obtain very good images of about half of the body at the maximum resolution of 60 m per pixel. From the images and radio-science experiment, a density of about (3.4±0.3) g/cm3 has been inferred for the asteroid. Many impact craters have been observed on the surface of Lutetia and the largest, named Massilia, has a diameter of about 55 km. Relative to the size of Lutetia (the longest axis is approximately 126 km) the crater represents one of the dominating features on its surface. Whether or not the impact that formed Massilia affected the entire asteroid can be only evaluated via numerical modeling, with hydrocodes, of the impact process. The results of a suite of iSALE simulations are compared with the crater profile derived from the Digital Terrain Model of the observed surface. The best match to the DTM of the crater with hydrocode simulations has allowed to determine a value of 7.5 km for the impactor diameter, which suggests a primordial origin of Lutetia due to the low probability of such an impact event. A second interesting impact structure has been identified nearby Massilia within the North Pole Crater Cluster. The crater has a diameter of 24 km and it lies over a larger crater of the North Pole Crater Cluster. This is strongly suggestive of a very young structure on Lutetia. The numerical simulations of this feature constrain the impactor to be 3.8 km in diameter, assuming the same material properties for target and impactor as in the model of the formation of Massilia. Article in Journal/Newspaper North Pole Unknown North Pole Planetary and Space Science 66 1 147 154
spellingShingle Asteroiden und Kometen
Cremonese, G.
Martellato, E.
Marzari, F.
Kührt, E.
Scholten, F.
Preusker, Frank
Wünnemann, K.
Borin, P.
Massironi, M.
Simoni, E.
Ip, W-H.
OSIRIS, team
Hydrocode simulations of the largest crater on asteroid Lutetia
title Hydrocode simulations of the largest crater on asteroid Lutetia
title_full Hydrocode simulations of the largest crater on asteroid Lutetia
title_fullStr Hydrocode simulations of the largest crater on asteroid Lutetia
title_full_unstemmed Hydrocode simulations of the largest crater on asteroid Lutetia
title_short Hydrocode simulations of the largest crater on asteroid Lutetia
title_sort hydrocode simulations of the largest crater on asteroid lutetia
topic Asteroiden und Kometen
topic_facet Asteroiden und Kometen
url https://elib.dlr.de/78590/