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Overview and Results From the Mars 2020 Perseverance Rover's First Science Campaign on the Jezero Crater Floor

Sun, Vivian Z. ; Hand, Kevin P. ; Stack, Kathryn M. ; Farley, Ken A. ; Simon, Justin I. ; Newman, Claire ; Sharma, Sunanda ; Liu, Yang ; Wiens, Roger C. and Williams, Amy J. , et al. (2023) In Journal of Geophysical Research: Planets 128(6).
Abstract

The Mars 2020 Perseverance rover landed in Jezero crater on 18 February 2021. After a 100-sol period of commissioning and the Ingenuity Helicopter technology demonstration, Perseverance began its first science campaign to explore the enigmatic Jezero crater floor, whose igneous or sedimentary origins have been much debated in the scientific community. This paper describes the campaign plan developed to explore the crater floor's Máaz and Séítah formations and summarizes the results of the campaign between sols 100–379. By the end of the campaign, Perseverance had traversed more than 5 km, created seven abrasion patches, and sealed nine samples and a witness tube. Analysis of remote and proximity science observations show that the Máaz... (More)

The Mars 2020 Perseverance rover landed in Jezero crater on 18 February 2021. After a 100-sol period of commissioning and the Ingenuity Helicopter technology demonstration, Perseverance began its first science campaign to explore the enigmatic Jezero crater floor, whose igneous or sedimentary origins have been much debated in the scientific community. This paper describes the campaign plan developed to explore the crater floor's Máaz and Séítah formations and summarizes the results of the campaign between sols 100–379. By the end of the campaign, Perseverance had traversed more than 5 km, created seven abrasion patches, and sealed nine samples and a witness tube. Analysis of remote and proximity science observations show that the Máaz and Séítah formations are igneous in origin and composed of five and two geologic members, respectively. The Séítah formation represents the olivine-rich cumulate formed from differentiation of a slowly cooling melt or magma body, and the Máaz formation likely represents a separate series of lava flows emplaced after Séítah. The Máaz and Séítah rocks also preserve evidence of multiple episodes of aqueous alteration in secondary minerals like carbonate, Fe/Mg phyllosilicates, sulfates, and perchlorate, and surficial coatings. Post-emplacement processes tilted the rocks near the Máaz-Séítah contact and substantial erosion modified the crater floor rocks to their present-day expressions. Results from this crater floor campaign, including those obtained upon return of the collected samples, will help to build the geologic history of events that occurred in Jezero crater and provide time constraints on the formation of the Jezero delta.

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organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
Jezero, Mars, Perseverance, rover
in
Journal of Geophysical Research: Planets
volume
128
issue
6
article number
e2022JE007613
publisher
Wiley-Blackwell
external identifiers
  • scopus:85163299408
ISSN
2169-9097
DOI
10.1029/2022JE007613
language
English
LU publication?
yes
id
d54ae37b-a56a-4da7-9dc4-9df1a5552680
date added to LUP
2023-09-15 13:38:51
date last changed
2023-09-15 13:38:51
@article{d54ae37b-a56a-4da7-9dc4-9df1a5552680,
  abstract     = {{<p>The Mars 2020 Perseverance rover landed in Jezero crater on 18 February 2021. After a 100-sol period of commissioning and the Ingenuity Helicopter technology demonstration, Perseverance began its first science campaign to explore the enigmatic Jezero crater floor, whose igneous or sedimentary origins have been much debated in the scientific community. This paper describes the campaign plan developed to explore the crater floor's Máaz and Séítah formations and summarizes the results of the campaign between sols 100–379. By the end of the campaign, Perseverance had traversed more than 5 km, created seven abrasion patches, and sealed nine samples and a witness tube. Analysis of remote and proximity science observations show that the Máaz and Séítah formations are igneous in origin and composed of five and two geologic members, respectively. The Séítah formation represents the olivine-rich cumulate formed from differentiation of a slowly cooling melt or magma body, and the Máaz formation likely represents a separate series of lava flows emplaced after Séítah. The Máaz and Séítah rocks also preserve evidence of multiple episodes of aqueous alteration in secondary minerals like carbonate, Fe/Mg phyllosilicates, sulfates, and perchlorate, and surficial coatings. Post-emplacement processes tilted the rocks near the Máaz-Séítah contact and substantial erosion modified the crater floor rocks to their present-day expressions. Results from this crater floor campaign, including those obtained upon return of the collected samples, will help to build the geologic history of events that occurred in Jezero crater and provide time constraints on the formation of the Jezero delta.</p>}},
  author       = {{Sun, Vivian Z. and Hand, Kevin P. and Stack, Kathryn M. and Farley, Ken A. and Simon, Justin I. and Newman, Claire and Sharma, Sunanda and Liu, Yang and Wiens, Roger C. and Williams, Amy J. and Tosca, Nicholas and Alwmark, Sanna and Beyssac, Olivier and Brown, Adrian and Calef, Fred and Cardarelli, Emily L. and Clavé, Elise and Cohen, Barbara and Corpolongo, Andrea and Czaja, Andrew D. and Del Sesto, Tyler and Fairen, Alberto and Fornaro, Teresa and Fouchet, Thierry and Garczynski, Brad and Gupta, Sanjeev and Herd, Chris D.K. and Hickman-Lewis, Keyron and Horgan, Briony and Johnson, Jeffrey and Kinch, Kjartan and Kizovski, Tanya and Kronyak, Rachel and Lange, Robert and Mandon, Lucia and Milkovich, Sarah and Moeller, Robert and Núñez, Jorge and Paar, Gerhard and Pyrzak, Guy and Quantin-Nataf, Cathy and Shuster, David L. and Siljestrom, Sandra and Steele, Andrew and Tice, Michael and Toupet, Olivier and Udry, Arya and Vaughan, Alicia and Wogsland, Brittan}},
  issn         = {{2169-9097}},
  keywords     = {{Jezero; Mars; Perseverance; rover}},
  language     = {{eng}},
  number       = {{6}},
  publisher    = {{Wiley-Blackwell}},
  series       = {{Journal of Geophysical Research: Planets}},
  title        = {{Overview and Results From the Mars 2020 Perseverance Rover's First Science Campaign on the Jezero Crater Floor}},
  url          = {{http://dx.doi.org/10.1029/2022JE007613}},
  doi          = {{10.1029/2022JE007613}},
  volume       = {{128}},
  year         = {{2023}},
}