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An overfilled lacustrine system and progradational delta in Jezero crater, Mars: Implications for Noachian climate
DOI: 10.1016/j.pss.2012.02.003 Bibcode: 2012P&SS...67...28S

Head, James W.; Fassett, Caleb I.; Schon, Samuel C.

The presence of valley networks and open-basin lakes in the late Noachian is cited as evidence for overland flow of liquid water and thus a climate on early Mars that might have supported precipitation and runoff. Outstanding questions center on the nature of such a climate, its duration and variability, and its cause. Open basin lakes, their inte…

2012 Planetary and Space Science
MEx 135
Applications of a new set of methane line parameters to the modeling of Titan’s spectrum in the 1.58 µm window
DOI: 10.1016/j.pss.2011.05.003 Bibcode: 2012P&SS...61...85D

Drossart, Pierre; Bézard, Bruno; Lellouch, Emmanuel +11 more

In this paper we apply a recently released set of methane line parameters (Wang et al., 2011) to the modeling of Titan spectra in the 1.58 µm window at both low and high spectral resolution. We first compare the methane absorption based on this new set of methane data to that calculated from the methane absorption coefficients derived in sit…

2012 Planetary and Space Science
Huygens 87
Titan’s internal structure and the evolutionary consequences
DOI: 10.1016/j.pss.2011.04.010 Bibcode: 2012P&SS...60...10F

Fortes, A. D.

Titan’s moment of inertia (MoI), estimated from the quadrupole gravity field measured by the Cassini spacecraft, is 0.342, which has been interpreted as evidence of a partially differentiated internal mass distribution. It is shown here that the observed MoI is equally consistent with a fully differentiated internal structure comprising a shell of…

2012 Planetary and Space Science
Cassini 79
Titan’s global crater population: A new assessment
DOI: 10.1016/j.pss.2011.02.016 Bibcode: 2012P&SS...60...26N

Lorenz, R. D.; Neish, C. D.

We report a revised crater population for Titan using Cassini RADAR data through January 2010 (flyby T65), and make a size-dependent correction for the incomplete coverage (∼33%) using a Monte-Carlo model. Qualitatively, Titan’s landscape is more heavily cratered than Earth, but much less than Mars or Ganymede: the area fraction covered by craters…

2012 Planetary and Space Science
Cassini 76
Titan's fluvial valleys: Morphology, distribution, and spectral properties
DOI: 10.1016/j.pss.2011.01.020 Bibcode: 2012P&SS...60...34L

Sotin, C.; Barnes, J. W.; Brown, R. H. +11 more

Titan's fluvial channels have been investigated based on data obtained by the Synthetic Aperture Radar (SAR) instrument and the Visible and Infrared Mapping Spectrometer (VIMS) onboard the Cassini spacecraft. In this paper, a database of fluvial features is created based on radar-SAR data aiming to unveil the distribution and the morphologic and s…

2012 Planetary and Space Science
Cassini 69
Hydrogen peroxide on Mars: Observations, interpretation and future plans
DOI: 10.1016/j.pss.2011.03.019 Bibcode: 2012P&SS...68....3E

Encrenaz, T.; Atreya, S. K.; Greathouse, T. K. +1 more

Ever since the Viking mass spectrometer failed to detect organics on the surface of Mars in 1976 (Biemann et al., 1976), hydrogen peroxide (H2O2) has been suggested as a possible oxidizer of the Martian surface (Oyama and Berdahl, 1977). However, the search for H2O2 on Mars was unsuccessful for three dec…

2012 Planetary and Space Science
MEx 67
Spatial and temporal variations in Titan's surface temperatures from Cassini CIRS observations
DOI: 10.1016/j.pss.2011.03.015 Bibcode: 2012P&SS...60...62C

Irwin, P. G. J.; Teanby, N. A.; de Kok, R. +4 more

We report a wide-ranging study of Titan's surface temperatures by analysis of the Moon's outgoing radiance through a spectral window in the thermal infrared at 19 µm (530 cm-1) characterized by lower atmospheric opacity. We begin by modeling Cassini Composite Infrared Spectrometer (CIRS) far infrared spectra collected in the perio…

2012 Planetary and Space Science
Cassini 60
Chronology of deposition and alteration in the Mawrth Vallis region, Mars
DOI: 10.1016/j.pss.2012.06.023 Bibcode: 2012P&SS...72...31L

Mangold, N.; Bibring, J. -P.; Loizeau, D. +2 more

The Mawrth Vallis area displays some of the largest phyllosilicate-rich outcrops of Mars, on Noachian highlands. The Mawrth Vallis region is located just at the dichotomy boundary between the Noachian highlands and the younger, northern lowlands. A large, thick, layered clay-rich unit is present throughout the inter-crater plateaus. Clay-rich laye…

2012 Planetary and Space Science
MEx 59
The Saturnian satellite Rhea as seen by Cassini VIMS
DOI: 10.1016/j.pss.2011.07.019 Bibcode: 2012P&SS...61..142S

Baines, Kevin H.; Buratti, Bonnie J.; Clark, Roger N. +16 more

Since the arrival of the Cassini spacecraft at Saturn in June 2004, the Visual and Infrared Mapping Spectrometer has obtained new spectral data of the icy satellites of Saturn in the spectral range from 0.35 to 5.2 µm. Numerous flybys were performed at Saturn’s second largest satellite Rhea, providing a nearly complete coverage with pixel-gr…

2012 Planetary and Space Science
Cassini 53
Late Hesperian aqueous alteration at Majuro crater, Mars
DOI: 10.1016/j.pss.2012.03.014 Bibcode: 2012P&SS...72...18M

Mangold, N.; Poulet, F.; Ansan, V. +3 more

Impact craters cover a large portion of the surface of Mars and could constitute a significant exobiology research target as their formation provided heat sources for aqueous processes. To date, only rare examples of hydrothermal alteration in craters have been reported on Mars while many studies have focused on modeling their effect. Using data f…

2012 Planetary and Space Science
MEx 51