Search Publications

The mineral diversity of Jezero crater: Evidence for possible lacustrine carbonates on Mars
DOI: 10.1016/j.icarus.2019.113526 Bibcode: 2020Icar..33913526H

Anderson, Ryan B.; Horgan, Briony H. N.; Dromart, Gilles +2 more

Noachian-aged Jezero crater is the only known location on Mars where clear orbital detections of carbonates are found in close proximity to clear fluvio-lacustrine features indicating the past presence of a paleolake; however, it is unclear whether or not the carbonates in Jezero are related to the lacustrine activity. This distinction is critical…

2020 Icarus
MEx 154
Geology of the InSight landing site on Mars
DOI: 10.1038/s41467-020-14679-1 Bibcode: 2020NatCo..11.1014G

Rodriguez, S.; Forget, F.; Hauber, E. +44 more

The Interior Exploration using Seismic Investigations, Geodesy and Heat Transport (InSight) spacecraft landed successfully on Mars and imaged the surface to characterize the surficial geology. Here we report on the geology and subsurface structure of the landing site to aid in situ geophysical investigations. InSight landed in a degraded impact cr…

2020 Nature Communications
MEx 100
Photogeologic Map of the Perseverance Rover Field Site in Jezero Crater Constructed by the Mars 2020 Science Team
DOI: 10.1007/s11214-020-00739-x Bibcode: 2020SSRv..216..127S

Liu, Yang; Mangold, Nicolas; Johnson, Jeffrey R. +64 more

The Mars 2020 Perseverance rover landing site is located within Jezero crater, a ∼50 km diameter impact crater interpreted to be a Noachian-aged lake basin inside the western edge of the Isidis impact structure. Jezero hosts remnants of a fluvial delta, inlet and outlet valleys, and infill deposits containing diverse carbonate, mafic, and hydrated…

2020 Space Science Reviews
MEx 77
Valley formation on early Mars by subglacial and fluvial erosion
DOI: 10.1038/s41561-020-0618-x Bibcode: 2020NatGe..13..663G

Osinski, Gordon R.; Grau Galofre, Anna; Jellinek, A. Mark

The southern highlands of Mars are dissected by hundreds of valley networks, which are evidence that water once sculpted the surface. Characterizing the mechanisms of valley incision may constrain early Mars climate and the search for ancient life. Previous interpretations of the geological record require precipitation and surface water runoff to …

2020 Nature Geoscience
MEx 56
Fluvial Regimes, Morphometry, and Age of Jezero Crater Paleolake Inlet Valleys and Their Exobiological Significance for the 2020 Rover Mission Landing Site
DOI: 10.1089/ast.2019.2132 Bibcode: 2020AsBio..20..994M

Mangold, Nicolas; Quantin-Nataf, Cathy; Massé, Marion +5 more

Jezero crater has been selected as the landing site for the Mars 2020 Perseverance rover, because it contains a paleolake with two fan-deltas, inlet and outlet valleys. Using the data from the High Resolution Stereo Camera (HRSC) and the High Resolution Imaging Science Experiment (HiRISE), we conducted a quantitative geomorphological study of the …

2020 Astrobiology
MEx 56
Refining the age, emplacement and alteration scenarios of the olivine-rich unit in the Nili Fossae region, Mars
DOI: 10.1016/j.icarus.2019.113436 Bibcode: 2020Icar..33613436M

Mangold, N.; Quantin-Nataf, C.; Millot, C. +8 more

The Nili Fossae region of Mars exhibits from remote sensing spectral data the largest exposures of olivine-rich materials on the planet. However, it is not clearly constrained how and when these terrains formed. Some of the proposed scenarios favor a mode of formation closely related to Isidis impact basin: either under intense effusive volcanism …

2020 Icarus
MEx 53
Mars' Ionopause: A Matter of Pressures
DOI: 10.1029/2020JA028145 Bibcode: 2020JGRA..12528145S

Holmstrom, Mats; Sánchez-Cano, Beatriz; Mayyasi, Majd +8 more

This study assesses under what circumstances the Martian ionopause is formed on the dayside, both in regions where there are strong crustal magnetic fields and areas where these fields are small (<30 nT). Multiple data sets from three MAVEN dayside deep dip campaigns are utilized between periapsis and 600-1,000 km, as well as solar wind observa…

2020 Journal of Geophysical Research (Space Physics)
MEx 48
OpenMARS: A global record of martian weather from 1999 to 2015
DOI: 10.1016/j.pss.2020.104962 Bibcode: 2020P&SS..18804962H

Holmes, James A.; Lewis, Stephen R.; Patel, Manish R.

The Open access to Mars Assimilated Remote Soundings (OpenMARS) dataset is a reanalysis product combining past spacecraft observations with a Mars Global Circulation Model (GCM). The OpenMARS product is a global surface/atmosphere reference database of surface and atmospheric properties for almost nine Mars years that can be used by Mars scientist…

2020 Planetary and Space Science
MEx 41
Crust stratigraphy and heterogeneities of the first kilometers at the dichotomy boundary in western Elysium Planitia and implications for InSight lander
DOI: 10.1016/j.icarus.2019.113511 Bibcode: 2020Icar..33813511P

Pan, Lu; Quantin-Nataf, Cathy; Tauzin, Benoit +9 more

InSight landed on Mars on November 26, 2018, in western Elysium Planitia. The Mars crust beneath the lander is subject to complex geologic history next to the great topographic and crustal dichotomy of Mars. Understanding this part of the Martian crust in the subsurface would aid future investigations of the internal structure of the planet based …

2020 Icarus
MEx 36
Synergistic Ground and Orbital Observations of Iron Oxides on Mt. Sharp and Vera Rubin Ridge
DOI: 10.1029/2019JE006294 Bibcode: 2020JGRE..12506294F

Arvidson, R. E.; Morris, R. V.; Pinet, P. +12 more

Visible/short-wave infrared spectral data from the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) show absorptions attributed to hematite at Vera Rubin ridge (VRR), a topographic feature on northwest Mt. Sharp. The goals of this study are to determine why absorptions caused by ferric iron are strongly visible from orbit at VRR and to…

2020 Journal of Geophysical Research (Planets)
MEx 33