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dc.contributor.authorQuantin‐Nataf, C
dc.contributor.authorAlwmark, S
dc.contributor.authorCalef, FJ
dc.contributor.authorLasue, J
dc.contributor.authorKinch, K
dc.contributor.authorStack, KM
dc.contributor.authorSun, V
dc.contributor.authorWilliams, NR
dc.contributor.authorDehouck, E
dc.contributor.authorMandon, L
dc.contributor.authorMangold, N
dc.contributor.authorBeyssac, O
dc.contributor.authorClave, E
dc.contributor.authorWalter, SHG
dc.contributor.authorSimon, JI
dc.contributor.authorAnnex, AM
dc.contributor.authorHorgan, B
dc.contributor.authorRice, James W
dc.contributor.authorShuster, D
dc.contributor.authorCohen, B
dc.contributor.authorKah, L
dc.contributor.authorSholes, Steven
dc.contributor.authorWeiss, BP
dc.date.accessioned2026-04-15T20:59:31Z
dc.date.available2026-04-15T20:59:31Z
dc.date.issued2023-06-06
dc.identifier.urihttps://hdl.handle.net/1721.1/165457
dc.description.abstractDuring the first year of NASA's Mars 2020 mission, Perseverance rover has investigated the dark crater floor unit of Jezero crater and four samples of this unit have been collected. The focus of this paper is to assess the potential of these samples to calibrate the crater‐based Martian chronology. We first review the previous estimation of crater‐based model age of this unit. Then, we investigate the impact crater density distribution across the floor unit. It reveals that the crater density is heterogeneous from areas which have been exposed to the bombardment during the last 3 Ga to areas very recently exposed to bombardment. It suggests a complex history of exposure to impact cratering. We also display evidence of several remnants of deposits on the top of the dark floor unit across Jezero below which the dark floor unit may have been buried. We propose the following scenario of burying/exhumation: the dark floor unit would have been initially buried below a unit that was a few tens of meters thick. This unit then gradually eroded away due to Aeolian processes from the northeast to the west, resulting in uneven exposure to impact bombardment over 3 Ga. A cratering model reproducing this scenario confirms the feasibility of this hypothesis. Due to the complexity of its exposure history, the Jezero dark crater floor unit will require additional detailed analysis to understand how the Mars 2020 mission samples of the crater floor can be used to inform the Martian cratering chronology.en_US
dc.language.isoen
dc.publisherAmerican Geophysical Unionen_US
dc.relation.isversionof10.1029/2022je007628en_US
dc.rightsArticle is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.en_US
dc.sourceAmerican Geophysical Unionen_US
dc.titleThe Complex Exhumation History of Jezero Crater Floor Unit and Its Implication for Mars Sample Returnen_US
dc.typeArticleen_US
dc.identifier.citationQuantin-Nataf, C., Alwmark, S., Calef, F. J., Lasue, J., Kinch, K., Stack, K. M., et al. (2023). The complex exhumation history of Jezero crater floor unit and its implication for Mars sample return. Journal of Geophysical Research: Planets, 128, e2022JE007628.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.relation.journalJournal of Geophysical Research: Planetsen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2026-04-15T20:50:05Z
dspace.orderedauthorsQuantin‐Nataf, C; Alwmark, S; Calef, FJ; Lasue, J; Kinch, K; Stack, KM; Sun, V; Williams, NR; Dehouck, E; Mandon, L; Mangold, N; Beyssac, O; Clave, E; Walter, SHG; Simon, JI; Annex, AM; Horgan, B; Rice, JW; Shuster, D; Cohen, B; Kah, L; Sholes, S; Weiss, BPen_US
dspace.date.submission2026-04-15T20:50:08Z
mit.journal.volume128en_US
mit.journal.issue6en_US
mit.licensePUBLISHER_POLICY
mit.metadata.statusAuthority Work and Publication Information Neededen_US


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