Consolmagno, G. J.; Golabek, G. J.; Turrini, D.; Jutzi, Martin; Sirono, S.; Svetsov, V.; Tsiganis, K. (2015). Is Vesta an intact and pristine protoplanet? Icarus, 254, pp. 190-201. Elsevier 10.1016/j.icarus.2015.03.029
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It is difficult to find a Vesta model of iron core, pyroxene and olivine-rich mantle, and HED crust that can match the joint constraints of (a) Vesta's density and core size as reported by the Dawn spacecraft team; (b) the chemical trends of the HED meteorites, including the depletion of sodium, the FeO abundance, and the trace element enrichments; and (c) the absence of exposed mantle material on Vesta's surface, among Vestoid asteroids, or in our collection of basaltic meteorites. These conclusions are based entirely on mass-balance and density arguments, independent of any particular formation scenario for the HED meteorites themselves. We suggest that Vesta either formed from source material with non-chondritic composition or underwent after its formation a radical physical alteration, possibly caused by collisional processes, that affected its global composition and interior structure. (C) 2015 Elsevier Inc. All rights reserved.
Item Type: |
Journal Article (Original Article) |
---|---|
Division/Institute: |
08 Faculty of Science > Physics Institute > Space Research and Planetary Sciences > Theoretical Astrophysics and Planetary Science (TAPS) 08 Faculty of Science > Physics Institute > Space Research and Planetary Sciences |
UniBE Contributor: |
Jutzi, Martin |
Subjects: |
500 Science > 520 Astronomy 500 Science > 530 Physics |
ISSN: |
0019-1035 |
Publisher: |
Elsevier |
Language: |
English |
Submitter: |
Katharina Weyeneth-Moser |
Date Deposited: |
15 Jun 2016 13:49 |
Last Modified: |
05 Dec 2022 14:56 |
Publisher DOI: |
10.1016/j.icarus.2015.03.029 |
Web of Science ID: |
000355022000016 |
BORIS DOI: |
10.7892/boris.81928 |
URI: |
https://boris.unibe.ch/id/eprint/81928 |