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Geomorphic evidence for former lobate debris aprons at low latitudes on Mars: Indicators of the Martian paleoclimate
DOI: 10.1029/2007JE002897 Bibcode: 2008JGRE..113.2007H

Neukum, G.; Hauber, E.; van Gasselt, S. +1 more

Circumferential depressions enclosing mesas and plateaus in the northern Kasei Valles and in the Tartarus Colles regions of Mars are interpreted as indicators of the former extent of lobate debris aprons, thought to be mixtures of ice and clastic particles. These former lobate debris aprons existed about 1 Ga ago and were embayed by lavas or other…

2008 Journal of Geophysical Research (Planets)
MEx 64
Geomorphic study of fluvial landforms on the northern Valles Marineris plateau, Mars
DOI: 10.1029/2007JE002985 Bibcode: 2008JGRE..113.8009M

Mangold, N.; Quantin, C.; Neukum, G. +2 more

Fluvial landforms are observed on the plateau near Echus Chasma and other locations on the Valles Marineris plateau using high resolution (10 to 50 m/pixel) Mars Express images and topography. Branching valleys have a 20- to 100-m deep V-shape profile typical of fluvial processes. Their incision occurred in a thin (<150 m) and weak, dark unit t…

2008 Journal of Geophysical Research (Planets)
MEx 59
Mobile lid convection beneath Enceladus' south polar terrain
DOI: 10.1029/2008JE003114 Bibcode: 2008JGRE..113.7009B

Barr, Amy C.

Enceladus' south polar region has a large heat flux, 55-110 mW m-2, that is spatially associated with cryovolcanic and tectonic activity. Tidal dissipation and vigorous convection in the underlying ice shell are possible sources of heat, however, prior predictions of the heat flux carried by stagnant lid convection range from F con…

2008 Journal of Geophysical Research (Planets)
Cassini 57
Titan's winter polar vortex structure revealed by chemical tracers
DOI: 10.1029/2008JE003218 Bibcode: 2008JGRE..11312003T

Irwin, P. G. J.; Teanby, N. A.; Calcutt, S. B. +10 more

The winter polar vortex on Saturn's largest moon Titan has profound effects on atmospheric circulation and chemistry and for the current northern midwinter season is the major dynamical feature of Titan's stratosphere and mesosphere. We use 2 years of observations from Cassini's composite infrared spectrometer to determine cross sections of five i…

2008 Journal of Geophysical Research (Planets)
Cassini 55
Mapping and interpretation of Sinlap crater on Titan using Cassini VIMS and RADAR data
DOI: 10.1029/2007JE002965 Bibcode: 2008JGRE..113.4003L

Sotin, Christophe; Barnes, Jason W.; Le Mouélic, Stéphane +15 more

Only a few impact craters have been unambiguously detected on Titan by the Cassini-Huygens mission. Among these, Sinlap is the only one that has been observed both by the RADAR and VIMS instruments. This paper describes observations at centimeter and infrared wavelengths which provide complementary information about the composition, topography, an…

2008 Journal of Geophysical Research (Planets)
Cassini 55
Geological context of water-altered minerals in Valles Marineris, Mars
DOI: 10.1029/2007JE003070 Bibcode: 2008JGRE..11312005C

Hynek, Brian M.; Chojnacki, Matthew

Greater than 15,000 km2 of the layered deposits within Valles Marineris are associated with water-altered minerals, yet their origin and history of alteration remain a mystery. There are numerous competing hypotheses for the formation of the interior layered deposits including aeolian, lacustrine, and volcanic. Recent orbiter spectrosco…

2008 Journal of Geophysical Research (Planets)
MEx 53
Stratigraphy and structure of interior layered deposits in west Candor Chasma, Mars, from High Resolution Stereo Camera (HRSC) stereo imagery and derived elevations
DOI: 10.1029/2007JE003053 Bibcode: 2008JGRE..11310008F

Scholten, F.; Neukum, G.; Hauber, E. +5 more

Interior layered deposits (ILDs) within western Candor Chasma were studied by mapping lithologies, measuring layer attitudes and comparing the stratigraphy of two adjacent mounds. Layering tends to dip in the same direction as the local topographic slope, although at different angles. Regionally consistent attitudes do exist, suggesting postdeposi…

2008 Journal of Geophysical Research (Planets)
MEx 52
Characterization of mesoscale gravity waves in the upper and lower clouds of Venus from VEX-VIRTIS images
DOI: 10.1029/2008JE003185 Bibcode: 2008JGRE..113.0B18P

Hueso, R.; Sánchez-Lavega, A.; Drossart, P. +3 more

Images obtained from the Visible and InfraRed Thermal Imaging Spectrometer (VIRTIS)-M instrument onboard Venus Express present visible trains of alternating bands of cloud brightness in two different layers: at the upper cloud tops (~66 km altitude) observed in the dayside hemisphere using reflected ultraviolet light (380 nm) and in the lower clou…

2008 Journal of Geophysical Research (Planets)
VenusExpress 50
Composition of the Venus mesosphere measured by Solar Occultation at Infrared on board Venus Express
DOI: 10.1029/2008JE003140 Bibcode: 2008JGRE..113.0B23V

Vandaele, A. C.; Montmessin, F.; Fedorova, A. +8 more

Solar Occultation at Infrared (SOIR), which is a part of the Spectroscopy for Investigation of Characteristics of the Atmosphere of Venus (SPICAV) instrument on board Venus Express, combines an echelle-grating spectrometer with an acoustooptical tunable filter. It performs solar occultation measurements in the IR region at a high spectral resoluti…

2008 Journal of Geophysical Research (Planets)
VenusExpress 49
Relative age of interior layered deposits in southwest Candor Chasma based on high-resolution structural mapping
DOI: 10.1029/2008JE003181 Bibcode: 2008JGRE..11312002O

Kirk, Randolph L.; McEwen, Alfred S.; Okubo, Chris H. +1 more

High-resolution topography generated from stereo HiRISE (High-Resolution Imaging Science Experiment) imagery reveals the meter-scale structure of interior layered deposits (ILD) in southwest Candor Chasma. This study seeks to determine the age of the local ILD relative to any normal faults that can be attributed to chasma formation. The study area…

2008 Journal of Geophysical Research (Planets)
MEx 47